Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal

Detalhes bibliográficos
Autor(a) principal: Hendriks, Frits
Data de Publicação: 2010
Outros Autores: Kellner, Thomas, Liebermann, Lutz
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10362/4678
Resumo: XRD-analyses of pelitic deposits of Upper Jurassic to Miocene age occuring in the eastern Algarve (Portugal), give evidence of the occurrence of detrital clay minerals of continental origin as well as of conspicuous neoformations of marine provenance. The vertical succession of clay-mineral associations indicates the existence of three distinctive evolutionary cycles which are thought to reflect tectonically controlled transgressive-regressive events.
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spelling Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of PortugalClay mineralsEastern AlgarveXRD-analyses of pelitic deposits of Upper Jurassic to Miocene age occuring in the eastern Algarve (Portugal), give evidence of the occurrence of detrital clay minerals of continental origin as well as of conspicuous neoformations of marine provenance. The vertical succession of clay-mineral associations indicates the existence of three distinctive evolutionary cycles which are thought to reflect tectonically controlled transgressive-regressive events.RUNHendriks, FritsKellner, ThomasLiebermann, Lutz2010-12-28T15:29:18Z2010-12-282010-12-28T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10362/4678enginfo: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:RCAAP2024-03-11T03:31:36Zoai:run.unl.pt:10362/4678Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T03:14:46.079168Repositório 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 Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
title Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
spellingShingle Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
Hendriks, Frits
Clay minerals
Eastern Algarve
title_short Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
title_full Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
title_fullStr Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
title_full_unstemmed Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
title_sort Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
author Hendriks, Frits
author_facet Hendriks, Frits
Kellner, Thomas
Liebermann, Lutz
author_role author
author2 Kellner, Thomas
Liebermann, Lutz
author2_role author
author
dc.contributor.none.fl_str_mv RUN
dc.contributor.author.fl_str_mv Hendriks, Frits
Kellner, Thomas
Liebermann, Lutz
dc.subject.por.fl_str_mv Clay minerals
Eastern Algarve
topic Clay minerals
Eastern Algarve
description XRD-analyses of pelitic deposits of Upper Jurassic to Miocene age occuring in the eastern Algarve (Portugal), give evidence of the occurrence of detrital clay minerals of continental origin as well as of conspicuous neoformations of marine provenance. The vertical succession of clay-mineral associations indicates the existence of three distinctive evolutionary cycles which are thought to reflect tectonically controlled transgressive-regressive events.
publishDate 2010
dc.date.none.fl_str_mv 2010-12-28T15:29:18Z
2010-12-28
2010-12-28T00:00:00Z
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10362/4678
url http://hdl.handle.net/10362/4678
dc.language.iso.fl_str_mv eng
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