Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - Scadenza 2-11-2021

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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

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[num_revisions] => 1 [current_revision_id] => 353991 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) ) [1] => Array ( [nid] => 84000 [access] => 1 [node] => stdClass Object ( [vid] => 375299 [uid] => 32 [title] => Esito del premio - Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 84000 [type] => allegato [language] => it [created] => 1637850200 [changed] => 1637850200 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1637850200 [revision_uid] => 32 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Esito del premio [format] => [safe_value] => Esito del premio ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 101066 [uid] => 32 [filename] => Esito premio Infineon IngEle 2021 per web.pdf [uri] => public://2021/Esito premio Infineon IngEle 2021 per web.pdf [filemime] => application/pdf [filesize] => 178068 [status] => 1 [timestamp] => 1637850195 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => stefano.zampieri [picture] => 0 [data] => a:2:{s:13:"form_build_id";s:48:"form-WsCySmos4vAVlyFhG6gU5T7knfAyqco8LxlocSU_yIA";s:14:"wysiwyg_status";a:1:{i:1;i:1;}} [num_revisions] => 1 [current_revision_id] => 375299 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) ) [#formatter] => node_reference_default [0] => Array ( [#type] => link [#title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [#href] => node/77610 [#options] => Array ( [entity_type] => node [entity] => stdClass Object ( [vid] => 353991 [uid] => 2032 [title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77610 [type] => allegato [language] => it [created] => 1620042028 [changed] => 1620042028 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620042028 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353991 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) ) ) [1] => Array ( [#type] => link [#title] => Esito del premio - Infineon Ingegneria Elettronica in memoria di Alessia Lovato [#href] => node/84000 [#options] => Array ( [entity_type] => node [entity] => stdClass Object ( [vid] => 375299 [uid] => 32 [title] => Esito del premio - Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 84000 [type] => allegato [language] => it [created] => 1637850200 [changed] => 1637850200 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1637850200 [revision_uid] => 32 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Esito del premio [format] => [safe_value] => Esito del premio ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 101066 [uid] => 32 [filename] => Esito premio Infineon IngEle 2021 per web.pdf [uri] => public://2021/Esito premio Infineon IngEle 2021 per web.pdf [filemime] => application/pdf [filesize] => 178068 [status] => 1 [timestamp] => 1637850195 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => stefano.zampieri [picture] => 0 [data] => a:2:{s:13:"form_build_id";s:48:"form-WsCySmos4vAVlyFhG6gU5T7knfAyqco8LxlocSU_yIA";s:14:"wysiwyg_status";a:1:{i:1;i:1;}} [num_revisions] => 1 [current_revision_id] => 375299 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) ) ) [field_accordion_state] => Array ( [#theme] => field [#weight] => -1 [#title] => Aperto/Chiuso [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_accordion_state [#field_type] => list_text [#field_translatable] => 0 [#entity_type] => node [#bundle] => elemento_accordion [#object] => stdClass Object ( [vid] => 353992 [uid] => 2032 [title] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - Scadenza 2-11-2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77611 [type] => elemento_accordion [language] => it [created] => 1620042035 [changed] => 1641989668 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989668 [revision_uid] => 2032 [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( [und] => Array ( [0] => Array ( [value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[safe_summary] => ) ) ) [field_accordion_state] => Array ( [und] => Array ( [0] => Array ( [value] => chiuso ) ) ) [field_allegato_element] => Array ( [und] => Array ( [0] => Array ( [nid] => 77610 [access] => 1 [node] => stdClass Object ( [vid] => 353991 [uid] => 2032 [title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77610 [type] => allegato [language] => it [created] => 1620042028 [changed] => 1620042028 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620042028 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353991 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) ) [1] => Array ( [nid] => 84000 [access] => 1 [node] => stdClass Object ( [vid] => 375299 [uid] => 32 [title] => Esito del premio - Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 84000 [type] => allegato [language] => it [created] => 1637850200 [changed] => 1637850200 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1637850200 [revision_uid] => 32 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Esito del premio [format] => [safe_value] => Esito del premio ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 101066 [uid] => 32 [filename] => Esito premio Infineon IngEle 2021 per web.pdf [uri] => public://2021/Esito premio Infineon IngEle 2021 per web.pdf [filemime] => application/pdf [filesize] => 178068 [status] => 1 [timestamp] => 1637850195 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => stefano.zampieri [picture] => 0 [data] => a:2:{s:13:"form_build_id";s:48:"form-WsCySmos4vAVlyFhG6gU5T7knfAyqco8LxlocSU_yIA";s:14:"wysiwyg_status";a:1:{i:1;i:1;}} [num_revisions] => 1 [current_revision_id] => 375299 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) ) ) [field_outline_level] => Array ( [und] => Array ( [0] => Array ( [value] => h3 ) ) ) [field_titolo_frontend] => Array ( [und] => Array ( [0] => Array ( [value] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - scadenza 2 novembre 2021 [format] => [safe_value] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - scadenza 2 novembre 2021 ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353992 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => chiuso ) ) [#formatter] => text_default [0] => Array ( [#markup] => chiuso ) ) [links] => Array ( [#theme] => links__node [#pre_render] => Array ( [0] => drupal_pre_render_links ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) [node] => Array ( [#theme] => links__node__node [#links] => Array ( [node-readmore] => Array ( [title] => Read more about Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - Scadenza 2-11-2021 [href] => node/77611 [html] => 1 [attributes] => Array ( [rel] => tag [title] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - Scadenza 2-11-2021 ) ) ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) ) ) [field_outline_level] => Array ( [#theme] => field [#weight] => 31 [#title] => Livello outline [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_outline_level [#field_type] => list_text [#field_translatable] => 0 [#entity_type] => node [#bundle] => elemento_accordion [#object] => stdClass Object ( [vid] => 353992 [uid] => 2032 [title] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - Scadenza 2-11-2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77611 [type] => elemento_accordion [language] => it [created] => 1620042035 [changed] => 1641989668 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989668 [revision_uid] => 2032 [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( [und] => Array ( [0] => Array ( [value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di laurea magistrale in “Ingegneria elettronica” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.

Domanda di partecipazione in Moodle

[safe_summary] => ) ) ) [field_accordion_state] => Array ( [und] => Array ( [0] => Array ( [value] => chiuso ) ) ) [field_allegato_element] => Array ( [und] => Array ( [0] => Array ( [nid] => 77610 [access] => 1 [node] => stdClass Object ( [vid] => 353991 [uid] => 2032 [title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77610 [type] => allegato [language] => it [created] => 1620042028 [changed] => 1620042028 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620042028 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353991 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) ) [1] => Array ( [nid] => 84000 [access] => 1 [node] => stdClass Object ( [vid] => 375299 [uid] => 32 [title] => Esito del premio - Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 84000 [type] => allegato [language] => it [created] => 1637850200 [changed] => 1637850200 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1637850200 [revision_uid] => 32 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Esito del premio [format] => [safe_value] => Esito del premio ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 101066 [uid] => 32 [filename] => Esito premio Infineon IngEle 2021 per web.pdf [uri] => public://2021/Esito premio Infineon IngEle 2021 per web.pdf [filemime] => application/pdf [filesize] => 178068 [status] => 1 [timestamp] => 1637850195 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => stefano.zampieri [picture] => 0 [data] => a:2:{s:13:"form_build_id";s:48:"form-WsCySmos4vAVlyFhG6gU5T7knfAyqco8LxlocSU_yIA";s:14:"wysiwyg_status";a:1:{i:1;i:1;}} [num_revisions] => 1 [current_revision_id] => 375299 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) ) ) [field_outline_level] => Array ( [und] => Array ( [0] => Array ( [value] => h3 ) ) ) [field_titolo_frontend] => Array ( [und] => Array ( [0] => Array ( [value] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - scadenza 2 novembre 2021 [format] => [safe_value] => Premi Infineon Ingegneria Elettronica in memoria di Alessia Lovato - scadenza 2 novembre 2021 ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353992 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => h3 ) ) [#formatter] => text_default [0] => Array ( [#markup] => h3 ) ) )

Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato

Array ( [field_titolo_frontend_all] => Array ( [#theme] => field [#weight] => -4 [#title] => Titolo frontend [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_titolo_frontend_all [#field_type] => text_long [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato [#object] => stdClass Object ( [vid] => 353991 [uid] => 2032 [title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77610 [type] => allegato [language] => it [created] => 1620042028 [changed] => 1620042028 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620042028 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353991 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) [#formatter] => text_default [0] => Array ( [#markup] => Bando ) ) [field_allegato_file] => Array ( [#theme] => field [#weight] => -3 [#title] => File [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_allegato_file [#field_type] => file [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato [#object] => stdClass Object ( [vid] => 353991 [uid] => 2032 [title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77610 [type] => allegato [language] => it [created] => 1620042028 [changed] => 1620042028 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620042028 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353991 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) [#formatter] => file_default [0] => Array ( [#theme] => file_link [#file] => stdClass Object ( [fid] => 92911 [uid] => 2032 [filename] => Bando Premio Infineon IngEle 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon IngEle 2021.doc.pdf [filemime] => application/pdf [filesize] => 224490 [status] => 1 [timestamp] => 1620042023 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [links] => Array ( [#theme] => links__node [#pre_render] => Array ( [0] => drupal_pre_render_links ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) [node] => Array ( [#theme] => links__node__node [#links] => Array ( [node-readmore] => Array ( [title] => Read more about Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato [href] => node/77610 [html] => 1 [attributes] => Array ( [rel] => tag [title] => Bando Infineon Ingegneria Elettronica in memoria di Alessia Lovato ) ) ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) ) ) )

Premi Infineon ICT for Internet and Multimedia - Scadenza 2-11-2021

Array ( [field_titolo_frontend] => Array ( [#theme] => field [#weight] => -4 [#title] => Titolo frontend [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_titolo_frontend [#field_type] => text_long [#field_translatable] => 0 [#entity_type] => node [#bundle] => elemento_accordion [#object] => stdClass Object ( [vid] => 353986 [uid] => 2032 [title] => Premi Infineon ICT for Internet and Multimedia - Scadenza 2-11-2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77609 [type] => elemento_accordion [language] => it [created] => 1620041798 [changed] => 1641989675 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989675 [revision_uid] => 2032 [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( [und] => Array ( [0] => Array ( [value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[safe_summary] => ) ) ) [field_accordion_state] => Array ( [und] => Array ( [0] => Array ( [value] => chiuso ) ) ) [field_allegato_element] => Array ( [und] => Array ( [0] => Array ( [nid] => 77608 [access] => 1 [node] => stdClass Object ( [vid] => 353985 [uid] => 2032 [title] => Bando Infineon ICT for Internet and Multimedia [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77608 [type] => allegato [language] => it [created] => 1620041795 [changed] => 1620041795 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620041795 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92910 [uid] => 2032 [filename] => Bando Premio Infineon ICT 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon ICT 2021.doc_0.pdf [filemime] => application/pdf [filesize] => 224300 [status] => 1 [timestamp] => 1620041790 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353985 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) ) [1] => Array ( [nid] => 83771 [access] => 1 [node] => stdClass Object ( [vid] => 374770 [uid] => 2032 [title] => Esito premio Infeneon ICT 2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 83771 [type] => allegato [language] => it [created] => 1637656903 [changed] => 1637656903 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1637656903 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Esito premio Infeneon ICT 2021 [format] => [safe_value] => Esito premio Infeneon ICT 2021 ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 100816 [uid] => 2032 [filename] => Esito premio Infineon ICT 2021 per web.pdf [uri] => public://2021/Esito premio Infineon ICT 2021 per web.pdf [filemime] => application/pdf [filesize] => 178613 [status] => 1 [timestamp] => 1637656899 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 374770 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) [2] => Array ( [nid] => 85116 [access] => 1 [node] => stdClass Object ( [vid] => 379158 [uid] => 2032 [title] => Curriculum vincitori - Infineon [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 85116 [type] => allegato [language] => it [created] => 1641989605 [changed] => 1641989605 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989605 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Curriculum vincitori [format] => [safe_value] => Curriculum vincitori ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 102256 [uid] => 2032 [filename] => Curriculum Vitae_VARDHARAJAN MONISHA_Redacted.pdf [uri] => public://2022/Curriculum Vitae_VARDHARAJAN MONISHA_Redacted.pdf [filemime] => application/pdf [filesize] => 73892 [status] => 1 [timestamp] => 1641989586 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2463 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) [1] => Array ( [fid] => 102257 [uid] => 2032 [filename] => curriculum_tomasella_Redacted.pdf [uri] => public://2022/curriculum_tomasella_Redacted.pdf [filemime] => application/pdf [filesize] => 468012 [status] => 1 [timestamp] => 1641989604 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2463 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 379158 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) ) ) [field_outline_level] => Array ( [und] => Array ( [0] => Array ( [value] => h3 ) ) ) [field_titolo_frontend] => Array ( [und] => Array ( [0] => Array ( [value] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 [format] => [safe_value] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353986 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 [format] => [safe_value] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 ) ) [#formatter] => text_default [0] => Array ( [#markup] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 ) ) [body] => Array ( [#theme] => field [#weight] => -3 [#title] => Body [#access] => 1 [#label_display] => hidden [#view_mode] => teaser [#language] => und [#field_name] => body [#field_type] => text_with_summary [#field_translatable] => 0 [#entity_type] => node [#bundle] => elemento_accordion [#object] => stdClass Object ( [vid] => 353986 [uid] => 2032 [title] => Premi Infineon ICT for Internet and Multimedia - Scadenza 2-11-2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77609 [type] => elemento_accordion [language] => it [created] => 1620041798 [changed] => 1641989675 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989675 [revision_uid] => 2032 [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( [und] => Array ( [0] => Array ( [value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[safe_summary] => ) ) ) [field_accordion_state] => Array ( [und] => Array ( [0] => Array ( [value] => chiuso ) ) ) [field_allegato_element] => Array ( [und] => Array ( [0] => Array ( [nid] => 77608 [access] => 1 [node] => stdClass Object ( [vid] => 353985 [uid] => 2032 [title] => Bando Infineon ICT for Internet and Multimedia [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77608 [type] => allegato [language] => it [created] => 1620041795 [changed] => 1620041795 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620041795 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92910 [uid] => 2032 [filename] => Bando Premio Infineon ICT 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon ICT 2021.doc_0.pdf [filemime] => application/pdf [filesize] => 224300 [status] => 1 [timestamp] => 1620041790 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353985 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) ) [1] => Array ( [nid] => 83771 [access] => 1 [node] => stdClass Object ( [vid] => 374770 [uid] => 2032 [title] => Esito premio Infeneon ICT 2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 83771 [type] => allegato [language] => it [created] => 1637656903 [changed] => 1637656903 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1637656903 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Esito premio Infeneon ICT 2021 [format] => [safe_value] => Esito premio Infeneon ICT 2021 ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 100816 [uid] => 2032 [filename] => Esito premio Infineon ICT 2021 per web.pdf [uri] => public://2021/Esito premio Infineon ICT 2021 per web.pdf [filemime] => application/pdf [filesize] => 178613 [status] => 1 [timestamp] => 1637656899 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 374770 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) [2] => Array ( [nid] => 85116 [access] => 1 [node] => stdClass Object ( [vid] => 379158 [uid] => 2032 [title] => Curriculum vincitori - Infineon [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 85116 [type] => allegato [language] => it [created] => 1641989605 [changed] => 1641989605 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989605 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Curriculum vincitori [format] => [safe_value] => Curriculum vincitori ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 102256 [uid] => 2032 [filename] => Curriculum Vitae_VARDHARAJAN MONISHA_Redacted.pdf [uri] => public://2022/Curriculum Vitae_VARDHARAJAN MONISHA_Redacted.pdf [filemime] => application/pdf [filesize] => 73892 [status] => 1 [timestamp] => 1641989586 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2463 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) [1] => Array ( [fid] => 102257 [uid] => 2032 [filename] => curriculum_tomasella_Redacted.pdf [uri] => public://2022/curriculum_tomasella_Redacted.pdf [filemime] => application/pdf [filesize] => 468012 [status] => 1 [timestamp] => 1641989604 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2463 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 379158 [is_current] => 1 [is_pending] => [revision_moderation] => ) ) ) ) [field_outline_level] => Array ( [und] => Array ( [0] => Array ( [value] => h3 ) ) ) [field_titolo_frontend] => Array ( [und] => Array ( [0] => Array ( [value] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 [format] => [safe_value] => Premi Infineon ICT for Internet and Multimedia - scadenza 2 novembre 2021 ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353986 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[safe_summary] => ) ) [#formatter] => text_summary_or_trimmed [0] => Array ( [#markup] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
) ) [field_allegato_element] => Array ( [#theme] => field [#weight] => -2 [#title] => Elemento allegato [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_allegato_element [#field_type] => node_reference [#field_translatable] => 0 [#entity_type] => node [#bundle] => elemento_accordion [#object] => stdClass Object ( [vid] => 353986 [uid] => 2032 [title] => Premi Infineon ICT for Internet and Multimedia - Scadenza 2-11-2021 [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77609 [type] => elemento_accordion [language] => it [created] => 1620041798 [changed] => 1641989675 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1641989675 [revision_uid] => 2032 [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( [und] => Array ( [0] => Array ( [value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[safe_summary] => ) ) ) [field_accordion_state] => Array ( [und] => Array ( [0] => Array ( [value] => chiuso ) ) ) [field_allegato_element] => Array ( [und] => Array ( [0] => Array ( [nid] => 77608 [access] => 1 [node] => stdClass Object ( [vid] => 353985 [uid] => 2032 [title] => Bando Infineon ICT for Internet and Multimedia [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77608 [type] => allegato [language] => it [created] => 1620041795 [changed] => 1620041795 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620041795 [revision_uid] => 2032 [taxonomy_vocabulary_2] => Array ( ) [taxonomy_vocabulary_8] => Array ( ) [body] => Array ( ) [field_titolo_frontend_all] => Array ( [und] => Array ( [0] => Array ( [value] => Bando [format] => [safe_value] => Bando ) ) ) [field_allegato_file] => Array ( [und] => Array ( [0] => Array ( [fid] => 92910 [uid] => 2032 [filename] => Bando Premio Infineon ICT 2021.doc.pdf [uri] => public://2021/Bando Premio Infineon ICT 2021.doc_0.pdf [filemime] => application/pdf [filesize] => 224300 [status] => 1 [timestamp] => 1620041790 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2408 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [name] => francesca.forzan [picture] => 0 [data] => b:0; 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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
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A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
[summary] => [format] => 2 [safe_value] =>
A chi è rivolto: studentesse e studenti di cittadinanza italiana o straniera che abbiano effettuato la pre-immatricolazione al corso di Laurea Magistrale in “ICT for Internet and Multimedia” presso l’Ateneo patavino per l’a.a. 2021/22.
Tipologia: due premi di studio, del valore di 5.000,00 euro ciascuno.
 
Domanda di partecipazione in Moodle
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Bando Infineon ICT for Internet and Multimedia

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University of Padua co-author of an important discovery on the relationship between clayey materials and earthquake

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

[summary] => [format] => 2 [safe_value] =>

The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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The clayey materials of the faults present in the subduction areas, that is, where a tectonic plate slides under another plate, retain a "water buffer" inside them. This means that they favor earthquakes potentially capable of causing tsunamis. This is the result of the study "Fluid pressurization and earthquake propagation in the Hikurangi subduction zone" conducted thanks to the collaboration between the Italian Istituto Nazionale di Geofisica e Vulcanologia, the Universities of Pisa and Padua, and the University College London, on some samples from the Hikurangi area in New Zealand. The work was published in Nature Communications.

To study the behavior of these clays coming from the fault, the researchers conducted experiments on the samples collected during the international drilling mission "Integrated Ocean Drilling Program 375" carried out in 2018 off the North Island of New Zealand, attended by Professor Francesca Meneghini of the University of Pisa, second author of the published work. In detail the samples of the rocks present inside the fault have been pulverized.

The powders have been tested in the High Pressure and High Temperature (HP-HT) Laboratory of the INGV through a sophisticated apparatus, SHIVA (Slow to High Velocity Apparatus), funded by the European Research Council on a project by Giulio Di Toro, University of  Padua and co-author of this study, and reproduces the "engine" of earthquakes (the fault) allowing to observe what happens to the interior of the earth's crust, with the deformations that the rock undergoes under high pressures. Inside SHIVA, the powders have been analyzed using a new method to retain the water inside them while they are deformed at the typical speeds of earthquakes". Through the control tests conducted on a material whose characteristics are known, a Carrara marble powder, the researchers came to the conclusion that these clays favor the seismic slip of the fault precisely because of their ability to retain water, a characteristic that makes them 'weak'. “When I decided to participate in the oceanographic expedition, says Francesca Meneghini, "I immediately contacted my colleagues from INGV and the University of Padua, with whom I have been collaborating for years. I was sure it was a unique opportunity to test the new experimental technique developed at the Institute and make a further contribution to our knowledge of seismic phenomena”.

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C'è anche Unipd nei mari della Nuova Zelanda per un'importante scoperta sui terremoti

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Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[summary] => [format] => 2 [safe_value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



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Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[summary] => [format] => 2 [safe_value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[safe_summary] => ) ) [#formatter] => text_summary_or_trimmed [0] => Array ( [#markup] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di oss

) ) [field_img_box_lancio_news] => Array ( [#theme] => field [#weight] => 0 [#title] => Immagine [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_img_box_lancio_news [#field_type] => image [#field_translatable] => 0 [#entity_type] => node [#bundle] => box_lancio_news [#object] => stdClass Object ( [vid] => 353977 [uid] => 13 [title] => C'è anche Unipd nei mari della Nuova Zelanda per un'importante scoperta sui terremoti [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77604 [type] => box_lancio_news [language] => it [created] => 1620035580 [changed] => 1620035777 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620035777 [revision_uid] => 13 [body] => Array ( [und] => Array ( [0] => Array ( [value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[summary] => [format] => 2 [safe_value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[safe_summary] => ) ) ) [field_date_box_lancio_news] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03T00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => date ) ) ) [field_etichetta_box_lancio_news] => Array ( ) [field_img_box_lancio_news] => Array ( [und] => Array ( [0] => Array ( [fid] => 92906 [uid] => 13 [filename] => n_mare.jpg [uri] => public://n_mare.jpg [filemime] => image/jpeg [filesize] => 208055 [status] => 1 [timestamp] => 1620035777 [type] => image [field_file_image_alt_text] => Array ( ) [field_file_image_title_text] => Array ( ) [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( [height] => 630 [width] => 1200 ) [height] => 630 [width] => 1200 [alt] => mare [title] => ) ) ) [field_link_alla_news] => Array ( ) [field_link_esterno_news] => Array ( ) [field_pagina_associata] => Array ( ) [field_link_etichetta] => Array ( ) [field_abstract_news] => Array ( [und] => Array ( [0] => Array ( [value] => Analizzati con un nuovo metodo i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Giulio Di Toro, dell’Università di Padova, è co-autore di questo studio [format] => [safe_value] => Analizzati con un nuovo metodo i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Giulio Di Toro, dell’Università di Padova, è co-autore di questo studio ) ) ) [field_allegato_news] => Array ( ) [field_categorie_news] => Array ( [und] => Array ( [0] => Array ( [tid] => 2264 ) ) ) [field_pub_date] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03T00:00:00 [value2] => 2021-08-28T00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => date ) ) ) [field_layout_news] => Array ( [und] => Array ( [0] => Array ( [value] => single ) ) ) [field_testo_opzionale_news] => Array ( ) [field_url_en_page] => Array ( ) [field_url_en_page_label] => Array ( ) [path] => Array ( [pathauto] => 1 ) [name] => chiara.mezzalira [picture] => 0 [data] => a:2:{s:13:"form_build_id";s:37:"form-e496b743db3766e42eb8a4d1ccc1c014";s:14:"wysiwyg_status";a:1:{i:1;i:1;}} [num_revisions] => 3 [current_revision_id] => 353977 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [fid] => 92906 [uid] => 13 [filename] => n_mare.jpg [uri] => public://n_mare.jpg [filemime] => image/jpeg [filesize] => 208055 [status] => 1 [timestamp] => 1620035777 [type] => image [field_file_image_alt_text] => Array ( ) [field_file_image_title_text] => Array ( ) [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( [height] => 630 [width] => 1200 ) [height] => 630 [width] => 1200 [alt] => mare [title] => ) ) [#formatter] => image [0] => Array ( [#theme] => image_formatter [#item] => Array ( [fid] => 92906 [uid] => 13 [filename] => n_mare.jpg [uri] => public://n_mare.jpg [filemime] => image/jpeg [filesize] => 208055 [status] => 1 [timestamp] => 1620035777 [type] => image [field_file_image_alt_text] => Array ( ) [field_file_image_title_text] => Array ( ) [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( [height] => 630 [width] => 1200 ) [height] => 630 [width] => 1200 [alt] => mare [title] => ) [#image_style] => [#path] => ) ) [field_abstract_news] => Array ( [#theme] => field [#weight] => 0 [#title] => Abstract [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_abstract_news [#field_type] => text_long [#field_translatable] => 0 [#entity_type] => node [#bundle] => box_lancio_news [#object] => stdClass Object ( [vid] => 353977 [uid] => 13 [title] => C'è anche Unipd nei mari della Nuova Zelanda per un'importante scoperta sui terremoti [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77604 [type] => box_lancio_news [language] => it [created] => 1620035580 [changed] => 1620035777 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620035777 [revision_uid] => 13 [body] => Array ( [und] => Array ( [0] => Array ( [value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[summary] => [format] => 2 [safe_value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



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Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



[summary] => [format] => 2 [safe_value] =>

Analizzati con un nuovo metodo presso i laboratori INGV i sedimenti argillosi provenienti dal margine di subduzione neozelandese di Hikurangi, zona in passato luogo di tsunami e terremoti. Le polveri sono state testate nel Laboratorio Alta Pressione e Alte Temperature (HP-HT) dell’INGV attraverso un sofisticato apparato, SHIVA (Slow to High Velocity Apparatus) finanziato dall’European Research Council su un progetto di Giulio Di Toro, dell’Università di Padova e co-autore di questo studio, e riproduce il “motore” dei terremoti (la faglia) permettendo di osservare quello che accade all’interno della crosta terrestre e le deformazioni subite dalla roccia sotto fortissime pressioni. All’interno di SHIVA, le polveri sono state analizzate attraverso un nuovo metodo che ha consentito di trattenere al loro interno l’acqua mentre erano deformate alle velocità tipiche dei terremoti.

I materiali argillosi delle faglie presenti nelle zone di subduzione, cioè dove una placca tettonica scivola al di sotto di un’altra placca, trattengono al loro interno un “cuscinetto d’acqua” e ciò fa sì che essi favoriscano terremoti potenzialmente capaci a provocare tsunami.  Questo è il risultato dello studio “Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone”, condotto grazie alla collaborazione tra l’Istituto Nazionale di Geofisica e Vulcanologia, le Università di Pisa e Padova, e la University College London, su alcuni campioni provenienti dalla zona di Hikurangi in Nuova Zelanda. Il lavoro è stato pubblicato di ‘Nature Communications’.

Attraverso i test di controllo condotti su un materiale le cui caratteristiche sono note, una polvere di marmo di Carrara, i ricercatori e le ricercatrici sono arrivati alla conclusione che queste argille favoriscono lo scorrimento sismico della faglia proprio a causa della loro capacità di trattenere acqua, caratteristica che le rende più ‘deboli’.

“Quando ho deciso di partecipare alla spedizione oceanografica”, racconta Francesca Meneghini (Università di Pisa), “ho subito contattato i colleghi dell’INGV e dell’Università di Padova, coi quali collaboro da anni, certa che fosse un’opportunità unica per testare la nuova tecnica sperimentale sviluppata all’Istituto e dare un ulteriore contributo alla nostra conoscenza dei fenomeni sismici”.



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2020RUA05 - Allegato 3 - Verbale 3 - Giudizi Analitici

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2020PO185 - Allegato 11 - Verbale 2 - Elenco candidati

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RICERCA - Dai mari della Nuova Zelanda una importante scoperta sul rapporto tra materiali argillosi e terremoti

Array ( [field_luogo_area_stampa] => Array ( [#theme] => field [#weight] => -4 [#title] => Luogo [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_luogo_area_stampa [#field_type] => text_long [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato_area_stampa [#object] => stdClass Object ( [vid] => 353969 [uid] => 8835 [title] => RICERCA - Dai mari della Nuova Zelanda una importante scoperta sul rapporto tra materiali argillosi e terremoti [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77601 [type] => allegato_area_stampa [language] => und [created] => 1620033415 [changed] => 1620033415 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620033415 [revision_uid] => 8835 [body] => Array ( ) [field_allegato_area_stampa] => Array ( [und] => Array ( [0] => Array ( [fid] => 92899 [uid] => 8835 [filename] => 20210503kkk.pdf [uri] => public://20210503kkk.pdf [filemime] => application/pdf [filesize] => 1925183 [status] => 1 [timestamp] => 1620033415 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [field_all_imm_area_stampa] => Array ( ) [field_data_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) ) [field_luogo_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) ) [name] => stampa [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353969 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) [#formatter] => text_default [0] => Array ( [#markup] => Padova ) ) [field_data_area_stampa] => Array ( [#theme] => field [#weight] => -3 [#title] => Data [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_data_area_stampa [#field_type] => datetime [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato_area_stampa [#object] => stdClass Object ( [vid] => 353969 [uid] => 8835 [title] => RICERCA - Dai mari della Nuova Zelanda una importante scoperta sul rapporto tra materiali argillosi e terremoti [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77601 [type] => allegato_area_stampa [language] => und [created] => 1620033415 [changed] => 1620033415 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620033415 [revision_uid] => 8835 [body] => Array ( ) [field_allegato_area_stampa] => Array ( [und] => Array ( [0] => Array ( [fid] => 92899 [uid] => 8835 [filename] => 20210503kkk.pdf [uri] => public://20210503kkk.pdf [filemime] => application/pdf [filesize] => 1925183 [status] => 1 [timestamp] => 1620033415 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [field_all_imm_area_stampa] => Array ( ) [field_data_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) ) [field_luogo_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) ) [name] => stampa [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353969 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) [#formatter] => date_default [0] => Array ( [#markup] => Lun, 03/05/2021 ) ) [field_allegato_area_stampa] => Array ( [#theme] => field [#weight] => -2 [#title] => Allegato [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_allegato_area_stampa [#field_type] => file [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato_area_stampa [#object] => stdClass Object ( [vid] => 353969 [uid] => 8835 [title] => RICERCA - Dai mari della Nuova Zelanda una importante scoperta sul rapporto tra materiali argillosi e terremoti [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77601 [type] => allegato_area_stampa [language] => und [created] => 1620033415 [changed] => 1620033415 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620033415 [revision_uid] => 8835 [body] => Array ( ) [field_allegato_area_stampa] => Array ( [und] => Array ( [0] => Array ( [fid] => 92899 [uid] => 8835 [filename] => 20210503kkk.pdf [uri] => public://20210503kkk.pdf [filemime] => application/pdf [filesize] => 1925183 [status] => 1 [timestamp] => 1620033415 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [field_all_imm_area_stampa] => Array ( ) [field_data_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) ) [field_luogo_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) ) [name] => stampa [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353969 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [fid] => 92899 [uid] => 8835 [filename] => 20210503kkk.pdf [uri] => public://20210503kkk.pdf [filemime] => application/pdf [filesize] => 1925183 [status] => 1 [timestamp] => 1620033415 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) [#formatter] => file_default [0] => Array ( [#theme] => file_link [#file] => stdClass Object ( [fid] => 92899 [uid] => 8835 [filename] => 20210503kkk.pdf [uri] => public://20210503kkk.pdf [filemime] => application/pdf [filesize] => 1925183 [status] => 1 [timestamp] => 1620033415 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [links] => Array ( [#theme] => links__node [#pre_render] => Array ( [0] => drupal_pre_render_links ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) [node] => Array ( [#theme] => links__node__node [#links] => Array ( [node-readmore] => Array ( [title] => Read more about RICERCA - Dai mari della Nuova Zelanda una importante scoperta sul rapporto tra materiali argillosi e terremoti [href] => node/77601 [html] => 1 [attributes] => Array ( [rel] => tag [title] => RICERCA - Dai mari della Nuova Zelanda una importante scoperta sul rapporto tra materiali argillosi e terremoti ) ) ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) ) ) )

ANNALISA OBOE E ROBERTO BENEDUCE SU VERITÀ E POTERE: LA PAROLA CRITICA DI ALTRE DONNE E ALTRI UOMINI

Array ( [field_luogo_area_stampa] => Array ( [#theme] => field [#weight] => -4 [#title] => Luogo [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_luogo_area_stampa [#field_type] => text_long [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato_area_stampa [#object] => stdClass Object ( [vid] => 353964 [uid] => 8835 [title] => ANNALISA OBOE E ROBERTO BENEDUCE SU VERITÀ E POTERE: LA PAROLA CRITICA DI ALTRE DONNE E ALTRI UOMINI [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77600 [type] => allegato_area_stampa [language] => und [created] => 1620031148 [changed] => 1620031148 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620031148 [revision_uid] => 8835 [body] => Array ( ) [field_allegato_area_stampa] => Array ( [und] => Array ( [0] => Array ( [fid] => 92898 [uid] => 8835 [filename] => 20210506 OBOE - BENEDUCE _.pdf [uri] => public://20210506 OBOE - BENEDUCE _.pdf [filemime] => application/pdf [filesize] => 417076 [status] => 1 [timestamp] => 1620031148 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [field_all_imm_area_stampa] => Array ( ) [field_data_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) ) [field_luogo_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) ) [name] => stampa [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353964 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) [#formatter] => text_default [0] => Array ( [#markup] => Padova ) ) [field_data_area_stampa] => Array ( [#theme] => field [#weight] => -3 [#title] => Data [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_data_area_stampa [#field_type] => datetime [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato_area_stampa [#object] => stdClass Object ( [vid] => 353964 [uid] => 8835 [title] => ANNALISA OBOE E ROBERTO BENEDUCE SU VERITÀ E POTERE: LA PAROLA CRITICA DI ALTRE DONNE E ALTRI UOMINI [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77600 [type] => allegato_area_stampa [language] => und [created] => 1620031148 [changed] => 1620031148 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620031148 [revision_uid] => 8835 [body] => Array ( ) [field_allegato_area_stampa] => Array ( [und] => Array ( [0] => Array ( [fid] => 92898 [uid] => 8835 [filename] => 20210506 OBOE - BENEDUCE _.pdf [uri] => public://20210506 OBOE - BENEDUCE _.pdf [filemime] => application/pdf [filesize] => 417076 [status] => 1 [timestamp] => 1620031148 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [field_all_imm_area_stampa] => Array ( ) [field_data_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) ) [field_luogo_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) ) [name] => stampa [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353964 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) [#formatter] => date_default [0] => Array ( [#markup] => Lun, 03/05/2021 ) ) [field_allegato_area_stampa] => Array ( [#theme] => field [#weight] => -2 [#title] => Allegato [#access] => 1 [#label_display] => above [#view_mode] => teaser [#language] => und [#field_name] => field_allegato_area_stampa [#field_type] => file [#field_translatable] => 0 [#entity_type] => node [#bundle] => allegato_area_stampa [#object] => stdClass Object ( [vid] => 353964 [uid] => 8835 [title] => ANNALISA OBOE E ROBERTO BENEDUCE SU VERITÀ E POTERE: LA PAROLA CRITICA DI ALTRE DONNE E ALTRI UOMINI [log] => [status] => 1 [comment] => 0 [promote] => 1 [sticky] => 0 [nid] => 77600 [type] => allegato_area_stampa [language] => und [created] => 1620031148 [changed] => 1620031148 [tnid] => 0 [translate] => 0 [revision_timestamp] => 1620031148 [revision_uid] => 8835 [body] => Array ( ) [field_allegato_area_stampa] => Array ( [und] => Array ( [0] => Array ( [fid] => 92898 [uid] => 8835 [filename] => 20210506 OBOE - BENEDUCE _.pdf [uri] => public://20210506 OBOE - BENEDUCE _.pdf [filemime] => application/pdf [filesize] => 417076 [status] => 1 [timestamp] => 1620031148 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [field_all_imm_area_stampa] => Array ( ) [field_data_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => 2021-05-03 00:00:00 [timezone] => Europe/Paris [timezone_db] => Europe/Paris [date_type] => datetime ) ) ) [field_luogo_area_stampa] => Array ( [und] => Array ( [0] => Array ( [value] => Padova [format] => [safe_value] => Padova ) ) ) [name] => stampa [picture] => 0 [data] => b:0; [num_revisions] => 1 [current_revision_id] => 353964 [is_current] => 1 [is_pending] => [revision_moderation] => [entity_view_prepared] => 1 ) [#items] => Array ( [0] => Array ( [fid] => 92898 [uid] => 8835 [filename] => 20210506 OBOE - BENEDUCE _.pdf [uri] => public://20210506 OBOE - BENEDUCE _.pdf [filemime] => application/pdf [filesize] => 417076 [status] => 1 [timestamp] => 1620031148 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) [#formatter] => file_default [0] => Array ( [#theme] => file_link [#file] => stdClass Object ( [fid] => 92898 [uid] => 8835 [filename] => 20210506 OBOE - BENEDUCE _.pdf [uri] => public://20210506 OBOE - BENEDUCE _.pdf [filemime] => application/pdf [filesize] => 417076 [status] => 1 [timestamp] => 1620031148 [type] => document [field_folder] => Array ( [und] => Array ( [0] => Array ( [tid] => 2048 ) ) ) [metadata] => Array ( ) [display] => 1 [description] => ) ) ) [links] => Array ( [#theme] => links__node [#pre_render] => Array ( [0] => drupal_pre_render_links ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) [node] => Array ( [#theme] => links__node__node [#links] => Array ( [node-readmore] => Array ( [title] => Read more about ANNALISA OBOE E ROBERTO BENEDUCE SU VERITÀ E POTERE: LA PAROLA CRITICA DI ALTRE DONNE E ALTRI UOMINI [href] => node/77600 [html] => 1 [attributes] => Array ( [rel] => tag [title] => ANNALISA OBOE E ROBERTO BENEDUCE SU VERITÀ E POTERE: LA PAROLA CRITICA DI ALTRE DONNE E ALTRI UOMINI ) ) ) [#attributes] => Array ( [class] => Array ( [0] => links [1] => inline ) ) ) ) )

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