Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications
Autor(a) principal: | |
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Data de Publicação: | 2023 |
Outros Autores: | , , , , , , , , , , , , |
Tipo de documento: | Artigo de conferência |
Idioma: | por |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10174/35352 |
Resumo: | Geochronological data from the pre-Mesozoic basement of the Lusitanian Basement (West of the Porto-Tomar Fault) was obtained. Results show a predominant Cadomian/Pan-African and Eburnean inheritance/source, placing this sector as a peri-Gondwanan domain. However, two major differences can be seen in the data: samples with a clear absence in Mesoproterozoic ages vs. samples with a clear presence of these ages and Silurian-Devonian ages. If the former show clear signs of affinity with the Ossa-Morena Zone, the latter are similar to the South Portuguese Zone, being one of the samples, probably deposited in the Middle-Upper Devonian, interpreted as having a mixed source. |
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Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implicationsGeochronological data from the pre-Mesozoic basement of the Lusitanian Basement (West of the Porto-Tomar Fault) was obtained. Results show a predominant Cadomian/Pan-African and Eburnean inheritance/source, placing this sector as a peri-Gondwanan domain. However, two major differences can be seen in the data: samples with a clear absence in Mesoproterozoic ages vs. samples with a clear presence of these ages and Silurian-Devonian ages. If the former show clear signs of affinity with the Ossa-Morena Zone, the latter are similar to the South Portuguese Zone, being one of the samples, probably deposited in the Middle-Upper Devonian, interpreted as having a mixed source.Universidade de Coimbra2023-07-24T14:25:47Z2023-07-242023-07-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjecthttp://hdl.handle.net/10174/35352http://hdl.handle.net/10174/35352porBENTO DOS SANTOS, T., CHICHORRO, M., CARVALHO, D., CACHAPUZ, P., SOLÁ, A.R., DANTAS, E., ROMÃO, J.M., MOREIRA, N., DIAS DA SILVA, I., CLAVIJO, E., DÍEZ-MONTES, A., VALVERDE, P., SANTOS, R.V., LINNEMANN U. (2023), Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications. XI Congresso Nacional de Geologia, Coimbra, 319-320.simnaonaondndndndndndndnafm@uevora.ptndndndndndndBento dos Santos, TelmoChichorro, MartimCarvalho, DiogoCachapuz, PedroSolá, RitaDantas, E.Romão, JoséMoreira, NoelDias da Silva, ÍcaroClavijo, EmílioDiez-Montes, AlejandroValverde, P.Santos, R.V.Linnemann, Ulfinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-03T19:38:53Zoai:dspace.uevora.pt:10174/35352Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:23:47.060013Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
title |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
spellingShingle |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications Bento dos Santos, Telmo |
title_short |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
title_full |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
title_fullStr |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
title_full_unstemmed |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
title_sort |
Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications |
author |
Bento dos Santos, Telmo |
author_facet |
Bento dos Santos, Telmo Chichorro, Martim Carvalho, Diogo Cachapuz, Pedro Solá, Rita Dantas, E. Romão, José Moreira, Noel Dias da Silva, Ícaro Clavijo, Emílio Diez-Montes, Alejandro Valverde, P. Santos, R.V. Linnemann, Ulf |
author_role |
author |
author2 |
Chichorro, Martim Carvalho, Diogo Cachapuz, Pedro Solá, Rita Dantas, E. Romão, José Moreira, Noel Dias da Silva, Ícaro Clavijo, Emílio Diez-Montes, Alejandro Valverde, P. Santos, R.V. Linnemann, Ulf |
author2_role |
author author author author author author author author author author author author author |
dc.contributor.author.fl_str_mv |
Bento dos Santos, Telmo Chichorro, Martim Carvalho, Diogo Cachapuz, Pedro Solá, Rita Dantas, E. Romão, José Moreira, Noel Dias da Silva, Ícaro Clavijo, Emílio Diez-Montes, Alejandro Valverde, P. Santos, R.V. Linnemann, Ulf |
description |
Geochronological data from the pre-Mesozoic basement of the Lusitanian Basement (West of the Porto-Tomar Fault) was obtained. Results show a predominant Cadomian/Pan-African and Eburnean inheritance/source, placing this sector as a peri-Gondwanan domain. However, two major differences can be seen in the data: samples with a clear absence in Mesoproterozoic ages vs. samples with a clear presence of these ages and Silurian-Devonian ages. If the former show clear signs of affinity with the Ossa-Morena Zone, the latter are similar to the South Portuguese Zone, being one of the samples, probably deposited in the Middle-Upper Devonian, interpreted as having a mixed source. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-07-24T14:25:47Z 2023-07-24 2023-07-01T00:00:00Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/conferenceObject |
format |
conferenceObject |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10174/35352 http://hdl.handle.net/10174/35352 |
url |
http://hdl.handle.net/10174/35352 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
BENTO DOS SANTOS, T., CHICHORRO, M., CARVALHO, D., CACHAPUZ, P., SOLÁ, A.R., DANTAS, E., ROMÃO, J.M., MOREIRA, N., DIAS DA SILVA, I., CLAVIJO, E., DÍEZ-MONTES, A., VALVERDE, P., SANTOS, R.V., LINNEMANN U. (2023), Geochronological data for the Pre-Mesozoic basement located west of the Porto-Tomar Fault: geodynamic implications. XI Congresso Nacional de Geologia, Coimbra, 319-320. sim nao nao nd nd nd nd nd nd nd nafm@uevora.pt nd nd nd nd nd nd |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.publisher.none.fl_str_mv |
Universidade de Coimbra |
publisher.none.fl_str_mv |
Universidade de Coimbra |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
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1799136719597993984 |