Publicação

Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar

Ver documento

Detalhes bibliográficos
Resumo:In the southern part of Tagus basin, North of paleozoic rocks of Valverde-Senhor das Chagas (near Alcácer do Sal) horst, a marine transgression has been recognized, Upper Serravallian, and maybe Lower Tortonian in age. There are no earlier marine deposits, and no younger ones are known either. Paleozoic behaved as a barrier separating two basins, distinct at least since Middle Miocene until Upper Pleistocene. Until now, both were regarded as a single entity, the so-called «Sado basin» Southwards (Alvalade basin) there has been a single transgression. It was assummed that it was the same one as the former. Indeed it is not definitely so. Later transgression accounts for Esbarrondadoiro Formation, whose deposits have been ascribed to Tortonian or even to Middle Miocene. However they are Upper Messinian to Lower Zanclean. Esbarrondadoiro Formation is younger than Lower Member of Cacela Formation in Algarve and, with even stronger reason, than the upper-most well dated marine levels in Tagus basin. Age of Miocene units dealt with here has been based on small mammals found in marine sands.
Autores principais:Antunes, M. Telles
Outros Autores:Mein, P.; Pais, João
Assunto:Messinian Mammals Glauconite K-Ar ages South of Portugal
Ano:2008
País:Portugal
Tipo de documento:artigo
Tipo de acesso:acesso aberto
Instituição associada:Universidade Nova de Lisboa
Idioma:português
Origem:Repositório Institucional da UNL
_version_ 1868982784962330624
author Antunes, M. Telles
author2 Mein, P.
Pais, João
author2_role author
author
author_facet Antunes, M. Telles
Mein, P.
Pais, João
author_role author
contributor_name_str_mv RUN
country_str PT
creators_json_txt [{\"Person.name\":\"Antunes, M. Telles\"},{\"Person.name\":\"Mein, P.\"},{\"Person.name\":\"Pais, João\"}]
datacite.contributors.contributor.contributorName.fl_str_mv RUN
datacite.creators.creator.creatorName.fl_str_mv Antunes, M. Telles
Mein, P.
Pais, João
datacite.date.Accepted.fl_str_mv 2008-08-13T00:00:00Z
datacite.date.available.fl_str_mv 2008-08-13T22:25:17Z
datacite.date.embargoed.fl_str_mv 2008-08-13T22:25:17Z
datacite.rights.fl_str_mv http://purl.org/coar/access_right/c_abf2
datacite.subjects.subject.fl_str_mv Messinian
Mammals
Glauconite
K-Ar ages
South of Portugal
datacite.titles.title.fl_str_mv Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
dc.contributor.none.fl_str_mv RUN
dc.creator.none.fl_str_mv Antunes, M. Telles
Mein, P.
Pais, João
dc.date.Accepted.fl_str_mv 2008-08-13T00:00:00Z
dc.date.available.fl_str_mv 2008-08-13T22:25:17Z
dc.date.embargoed.fl_str_mv 2008-08-13T22:25:17Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv http://hdl.handle.net/10362/1545
dc.language.none.fl_str_mv por
dc.rights.none.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.subject.none.fl_str_mv Messinian
Mammals
Glauconite
K-Ar ages
South of Portugal
dc.title.fl_str_mv Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
dc.type.none.fl_str_mv http://purl.org/coar/resource_type/c_6501
description In the southern part of Tagus basin, North of paleozoic rocks of Valverde-Senhor das Chagas (near Alcácer do Sal) horst, a marine transgression has been recognized, Upper Serravallian, and maybe Lower Tortonian in age. There are no earlier marine deposits, and no younger ones are known either. Paleozoic behaved as a barrier separating two basins, distinct at least since Middle Miocene until Upper Pleistocene. Until now, both were regarded as a single entity, the so-called «Sado basin» Southwards (Alvalade basin) there has been a single transgression. It was assummed that it was the same one as the former. Indeed it is not definitely so. Later transgression accounts for Esbarrondadoiro Formation, whose deposits have been ascribed to Tortonian or even to Middle Miocene. However they are Upper Messinian to Lower Zanclean. Esbarrondadoiro Formation is younger than Lower Member of Cacela Formation in Algarve and, with even stronger reason, than the upper-most well dated marine levels in Tagus basin. Age of Miocene units dealt with here has been based on small mammals found in marine sands.
dirty 0
eu_rights_str_mv openAccess
format article
fulltext.url.fl_str_mv https://run.unl.pt/bitstreams/8e8fec22-1773-48d9-8c37-91ed001f1b27/download
id run_db38efbcd7dde20ed5fd46d95da4438e
identifier.url.fl_str_mv http://hdl.handle.net/10362/1545
inst_facet_str urn:organizationAcronym:unl{{{_:::_}}}Universidade Nova de Lisboa
instacron_str unl
institution Universidade Nova de Lisboa
instname_str Universidade Nova de Lisboa
language por
network_acronym_str run
network_name_str Repositório Institucional da UNL
oai_identifier_str oai:run.unl.pt:10362/1545
organization_str_mv urn:organizationAcronym:unl
person_str_mv Antunes, M. Telles
Mein, P.
Pais, João
publishDate 2008
repo_facet_str urn:repositoryAcronym:run{{{_:::_}}}Repositório Institucional da UNL
reponame_str Repositório Institucional da UNL
repository_id_str urn:repositoryAcronym:run
service_str_mv urn:repositoryAcronym:run
spelling porenIn the southern part of Tagus basin, North of paleozoic rocks of Valverde-Senhor das Chagas (near Alcácer do Sal) horst, a marine transgression has been recognized, Upper Serravallian, and maybe Lower Tortonian in age. There are no earlier marine deposits, and no younger ones are known either. Paleozoic behaved as a barrier separating two basins, distinct at least since Middle Miocene until Upper Pleistocene. Until now, both were regarded as a single entity, the so-called «Sado basin» Southwards (Alvalade basin) there has been a single transgression. It was assummed that it was the same one as the former. Indeed it is not definitely so. Later transgression accounts for Esbarrondadoiro Formation, whose deposits have been ascribed to Tortonian or even to Middle Miocene. However they are Upper Messinian to Lower Zanclean. Esbarrondadoiro Formation is younger than Lower Member of Cacela Formation in Algarve and, with even stronger reason, than the upper-most well dated marine levels in Tagus basin. Age of Miocene units dealt with here has been based on small mammals found in marine sands.application/pdfenDepósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-ArAntunes, M. TellesMein, P.Pais, JoãoHostingInstitutionOrganizationalRUNe-mailmailto:run@unl.ptrun@unl.pt2008-08-13T22:25:17Z2008-08-132008-08-13T00:00:00ZHandlehttp://hdl.handle.net/10362/1545http://purl.org/coar/access_right/c_abf2open accessMessinianMammalsGlauconiteK-Ar agesSouth of Portugal3578505 bytesliteraturehttp://purl.org/coar/resource_type/c_6501journal articlehttp://purl.org/coar/access_right/c_abf2application/pdffulltexthttps://run.unl.pt/bitstreams/8e8fec22-1773-48d9-8c37-91ed001f1b27/download
spellingShingle Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
Antunes, M. Telles
Messinian
Mammals
Glauconite
K-Ar ages
South of Portugal
status SINGLETON
subject.fl_str_mv Messinian
Mammals
Glauconite
K-Ar ages
South of Portugal
title Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
title_full Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
title_fullStr Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
title_full_unstemmed Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
title_short Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
title_sort Depósitos messinianos do sul de Portugal, mamíferos (incluindo Rodentia e Logomorpha) e idades K-Ar
topic Messinian
Mammals
Glauconite
K-Ar ages
South of Portugal
topic_facet Messinian
Mammals
Glauconite
K-Ar ages
South of Portugal
url http://hdl.handle.net/10362/1545
visible 1