Integração de métodos geofísicos na modelagem crustal da Bacia de Santos

Detalhes bibliográficos
Autor(a) principal: De Mio, Eduardo
Data de Publicação: 2005
Outros Autores: Chang, Hung Kiang [UNESP], Corrêa, Fernando Santos [UNESP]
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://hdl.handle.net/11449/224989
Resumo: The Santos Basin is a passive margin basin generated during the Neocominian, associated with Gondwana breakup event. The thickness of the sedimentary package reaches 15 km, including rift sequence deposited over thinned crust which originally was 35 km thick. Crustal modeling was performed over 8 lines aiming to recognize the rift phase geometry and estimate the amount of crustal stretching. The database used was: four depth converted seismic horizons, magnetic and gravimetric grids and depth to magnetic basement data. Pronounced crustal stretching has been recognized in the basin (crustal stretching factors ranging from 1.2 to 3.1), evidencing large deformation accommodation. The modeling results demand thick and widespreading volcanic layers to fit the model. These wedge shaped volcanic fill, bordered with normal faults, are a common feature in rift basins. Modeling results were confronted with depth to magnetic basement data, previously obtained, exhibiting strong correlation, mostly in shallow areas. © 2005 Sociedade Brasileira de Geofísica.
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spelling Integração de métodos geofísicos na modelagem crustal da Bacia de SantosIntegration of the geophysical methods in crustal modeling of the Santos basinCrustal modelingCrustal stretchingSantos BasinThe Santos Basin is a passive margin basin generated during the Neocominian, associated with Gondwana breakup event. The thickness of the sedimentary package reaches 15 km, including rift sequence deposited over thinned crust which originally was 35 km thick. Crustal modeling was performed over 8 lines aiming to recognize the rift phase geometry and estimate the amount of crustal stretching. The database used was: four depth converted seismic horizons, magnetic and gravimetric grids and depth to magnetic basement data. Pronounced crustal stretching has been recognized in the basin (crustal stretching factors ranging from 1.2 to 3.1), evidencing large deformation accommodation. The modeling results demand thick and widespreading volcanic layers to fit the model. These wedge shaped volcanic fill, bordered with normal faults, are a common feature in rift basins. Modeling results were confronted with depth to magnetic basement data, previously obtained, exhibiting strong correlation, mostly in shallow areas. © 2005 Sociedade Brasileira de Geofísica.Beicip Franlab, Av. Napoléon Bonaparte, 232, 92502 Rueil Malmaison CedexLEBAC - Laboratório de Estudo de Baclas Instituto de Geociências Universidade Estadual Paulista - UNESP, Av 24A, n 1515, Bairro Bela Vista, 13506-900 Rio Claro, São PauloLEBAC - Laboratório de Estudo de Baclas Instituto de Geociências Universidade Estadual Paulista - UNESP, Av 24A, n 1515, Bairro Bela Vista, 13506-900 Rio Claro, São PauloFranlabUniversidade Estadual Paulista (UNESP)De Mio, EduardoChang, Hung Kiang [UNESP]Corrêa, Fernando Santos [UNESP]2022-04-28T20:34:41Z2022-04-28T20:34:41Z2005-07-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article275-284Revista Brasileira de Geofisica, v. 23, n. 3, p. 275-284, 2005.0102-261Xhttp://hdl.handle.net/11449/2249892-s2.0-35948997694Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPporRevista Brasileira de Geofisicainfo:eu-repo/semantics/openAccess2022-04-28T20:34:41Zoai:repositorio.unesp.br:11449/224989Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T15:24:08.456464Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
Integration of the geophysical methods in crustal modeling of the Santos basin
title Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
spellingShingle Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
De Mio, Eduardo
Crustal modeling
Crustal stretching
Santos Basin
title_short Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
title_full Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
title_fullStr Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
title_full_unstemmed Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
title_sort Integração de métodos geofísicos na modelagem crustal da Bacia de Santos
author De Mio, Eduardo
author_facet De Mio, Eduardo
Chang, Hung Kiang [UNESP]
Corrêa, Fernando Santos [UNESP]
author_role author
author2 Chang, Hung Kiang [UNESP]
Corrêa, Fernando Santos [UNESP]
author2_role author
author
dc.contributor.none.fl_str_mv Franlab
Universidade Estadual Paulista (UNESP)
dc.contributor.author.fl_str_mv De Mio, Eduardo
Chang, Hung Kiang [UNESP]
Corrêa, Fernando Santos [UNESP]
dc.subject.por.fl_str_mv Crustal modeling
Crustal stretching
Santos Basin
topic Crustal modeling
Crustal stretching
Santos Basin
description The Santos Basin is a passive margin basin generated during the Neocominian, associated with Gondwana breakup event. The thickness of the sedimentary package reaches 15 km, including rift sequence deposited over thinned crust which originally was 35 km thick. Crustal modeling was performed over 8 lines aiming to recognize the rift phase geometry and estimate the amount of crustal stretching. The database used was: four depth converted seismic horizons, magnetic and gravimetric grids and depth to magnetic basement data. Pronounced crustal stretching has been recognized in the basin (crustal stretching factors ranging from 1.2 to 3.1), evidencing large deformation accommodation. The modeling results demand thick and widespreading volcanic layers to fit the model. These wedge shaped volcanic fill, bordered with normal faults, are a common feature in rift basins. Modeling results were confronted with depth to magnetic basement data, previously obtained, exhibiting strong correlation, mostly in shallow areas. © 2005 Sociedade Brasileira de Geofísica.
publishDate 2005
dc.date.none.fl_str_mv 2005-07-01
2022-04-28T20:34:41Z
2022-04-28T20:34:41Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv Revista Brasileira de Geofisica, v. 23, n. 3, p. 275-284, 2005.
0102-261X
http://hdl.handle.net/11449/224989
2-s2.0-35948997694
identifier_str_mv Revista Brasileira de Geofisica, v. 23, n. 3, p. 275-284, 2005.
0102-261X
2-s2.0-35948997694
url http://hdl.handle.net/11449/224989
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv Revista Brasileira de Geofisica
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 275-284
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
_version_ 1808128509509369856

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