Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography

Detalhes bibliográficos
Autor(a) principal: Machado, Gil
Data de Publicação: 2020
Outros Autores: Moreira, Noel, Silvério, Gonçalo
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/31493
Resumo: The Devonian sedimentary record of the Ossa-Morena Zone is scarce. In its southwestern domains, the Odivelas Limestone and correlatable units represent the single evidence of latest Early Devonian to Middle Devonia n (possibly into Frasnian) sedimentation in this area. Reefal and perireefa l sediments are frequently, but not always, associated to coeval volcanic rocks that probably supported atoll-like systems on the top of volcanic edifices. The northernmost occurrences are spatially associated with mississippian volcani c-sedimentary complexes. Their geometrical relation is still unclear, the limestones are possibly embedded as olitoliths, but can also be tectonically imbricated or simply reflecting draping of younger sediments around and above older (Devonian) sea-bed topography.
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spelling Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and PaleogeographyThe Devonian sedimentary record of the Ossa-Morena Zone is scarce. In its southwestern domains, the Odivelas Limestone and correlatable units represent the single evidence of latest Early Devonian to Middle Devonia n (possibly into Frasnian) sedimentation in this area. Reefal and perireefa l sediments are frequently, but not always, associated to coeval volcanic rocks that probably supported atoll-like systems on the top of volcanic edifices. The northernmost occurrences are spatially associated with mississippian volcani c-sedimentary complexes. Their geometrical relation is still unclear, the limestones are possibly embedded as olitoliths, but can also be tectonically imbricated or simply reflecting draping of younger sediments around and above older (Devonian) sea-bed topography.Comunicações Geológicas2022-03-29T14:41:20Z2022-03-292020-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://hdl.handle.net/10174/31493http://hdl.handle.net/10174/31493engMACHADO, G., MOREIRA, N., SILVÉRIO, G. (2020), Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography. Comunicações Geológicas, 107(I) (volume especial do X CNG), 43-47.https://www.lneg.pt/wp-content/uploads/2020/09/09_Machado-et-al.pdfgil.machado@chronosurveys.comnafm@uevora.comgoncalo.silverio@sapo.ptMachado, GilMoreira, NoelSilvério, Gonçaloinfo: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:RCAAP2024-01-03T19:30:56Zoai:dspace.uevora.pt:10174/31493Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:20:33.249709Repositório 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 Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
title Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
spellingShingle Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
Machado, Gil
title_short Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
title_full Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
title_fullStr Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
title_full_unstemmed Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
title_sort Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography
author Machado, Gil
author_facet Machado, Gil
Moreira, Noel
Silvério, Gonçalo
author_role author
author2 Moreira, Noel
Silvério, Gonçalo
author2_role author
author
dc.contributor.author.fl_str_mv Machado, Gil
Moreira, Noel
Silvério, Gonçalo
description The Devonian sedimentary record of the Ossa-Morena Zone is scarce. In its southwestern domains, the Odivelas Limestone and correlatable units represent the single evidence of latest Early Devonian to Middle Devonia n (possibly into Frasnian) sedimentation in this area. Reefal and perireefa l sediments are frequently, but not always, associated to coeval volcanic rocks that probably supported atoll-like systems on the top of volcanic edifices. The northernmost occurrences are spatially associated with mississippian volcani c-sedimentary complexes. Their geometrical relation is still unclear, the limestones are possibly embedded as olitoliths, but can also be tectonically imbricated or simply reflecting draping of younger sediments around and above older (Devonian) sea-bed topography.
publishDate 2020
dc.date.none.fl_str_mv 2020-01-01T00:00:00Z
2022-03-29T14:41:20Z
2022-03-29
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 http://hdl.handle.net/10174/31493
http://hdl.handle.net/10174/31493
url http://hdl.handle.net/10174/31493
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv MACHADO, G., MOREIRA, N., SILVÉRIO, G. (2020), Devonian Sedimentation in the SW boundary of the Ossa-Morena Zone: State of Art and Paleogeography. Comunicações Geológicas, 107(I) (volume especial do X CNG), 43-47.
https://www.lneg.pt/wp-content/uploads/2020/09/09_Machado-et-al.pdf
gil.machado@chronosurveys.com
nafm@uevora.com
goncalo.silverio@sapo.pt
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