Plio-pleistocene boundary: Olhos de Água oucrop

Detalhes bibliográficos
Autor(a) principal: Moura, Delminda
Data de Publicação: 2009
Outros Autores: Boski, T.
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10400.1/2676
Resumo: The occurrence of rocky and sandy cliffs on the south coast of the Algarve is a consequence of tectonic movement since the Upper Miocene. The Algarve Basin was affected by uplift west of Olhos de Água and subsidence to the east. This process created local sedimentary basins in the easternmost part of the Algarve which filled with sediment throughout the Pliocene and Pleistocene (Moura & Boski, 1999). In contrast to the carbonate sediments formed on the continental shelf during the Miocene, the Pliocene and Pleistocene sediments are mostly siliclastic, deposited in littoral and continental environments. Rapid uplift and consequent erosion produced abundant clastic sediments, which were carried into the regional sedimentary basins.
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spelling Plio-pleistocene boundary: Olhos de Água oucropPliocenoPleistocenoSedimentarMagnetostratigrafiaAlgarveThe occurrence of rocky and sandy cliffs on the south coast of the Algarve is a consequence of tectonic movement since the Upper Miocene. The Algarve Basin was affected by uplift west of Olhos de Água and subsidence to the east. This process created local sedimentary basins in the easternmost part of the Algarve which filled with sediment throughout the Pliocene and Pleistocene (Moura & Boski, 1999). In contrast to the carbonate sediments formed on the continental shelf during the Miocene, the Pliocene and Pleistocene sediments are mostly siliclastic, deposited in littoral and continental environments. Rapid uplift and consequent erosion produced abundant clastic sediments, which were carried into the regional sedimentary basins.CIMA – Centro de Investigação Marinha e AmbientalSapientiaMoura, DelmindaBoski, T.2013-04-29T11:21:07Z20092009-01-01T00:00:00Zbook partinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/10400.1/2676eng978-989-95636-5-0AUT: DMO00293;info: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:RCAAP2024-11-29T10:37:20Zoai:sapientia.ualg.pt:10400.1/2676Portal AgregadorONGhttps://www.rcaap.pt/oai/openairemluisa.alvim@gmail.comopendoar:71602024-11-29T10:37:20Repositório 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 Plio-pleistocene boundary: Olhos de Água oucrop
title Plio-pleistocene boundary: Olhos de Água oucrop
spellingShingle Plio-pleistocene boundary: Olhos de Água oucrop
Moura, Delminda
Plioceno
Pleistoceno
Sedimentar
Magnetostratigrafia
Algarve
title_short Plio-pleistocene boundary: Olhos de Água oucrop
title_full Plio-pleistocene boundary: Olhos de Água oucrop
title_fullStr Plio-pleistocene boundary: Olhos de Água oucrop
title_full_unstemmed Plio-pleistocene boundary: Olhos de Água oucrop
title_sort Plio-pleistocene boundary: Olhos de Água oucrop
author Moura, Delminda
author_facet Moura, Delminda
Boski, T.
author_role author
author2 Boski, T.
author2_role author
dc.contributor.none.fl_str_mv Sapientia
dc.contributor.author.fl_str_mv Moura, Delminda
Boski, T.
dc.subject.por.fl_str_mv Plioceno
Pleistoceno
Sedimentar
Magnetostratigrafia
Algarve
topic Plioceno
Pleistoceno
Sedimentar
Magnetostratigrafia
Algarve
description The occurrence of rocky and sandy cliffs on the south coast of the Algarve is a consequence of tectonic movement since the Upper Miocene. The Algarve Basin was affected by uplift west of Olhos de Água and subsidence to the east. This process created local sedimentary basins in the easternmost part of the Algarve which filled with sediment throughout the Pliocene and Pleistocene (Moura & Boski, 1999). In contrast to the carbonate sediments formed on the continental shelf during the Miocene, the Pliocene and Pleistocene sediments are mostly siliclastic, deposited in littoral and continental environments. Rapid uplift and consequent erosion produced abundant clastic sediments, which were carried into the regional sedimentary basins.
publishDate 2009
dc.date.none.fl_str_mv 2009
2009-01-01T00:00:00Z
2013-04-29T11:21:07Z
dc.type.driver.fl_str_mv book part
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.1/2676
url http://hdl.handle.net/10400.1/2676
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 978-989-95636-5-0
AUT: DMO00293;
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv CIMA – Centro de Investigação Marinha e Ambiental
publisher.none.fl_str_mv CIMA – Centro de Investigação Marinha e Ambiental
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
repository.mail.fl_str_mv mluisa.alvim@gmail.com
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