Publicação
Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean
| Resumo: | The extensional process affecting Iberia during the Triassic and Jurassic times change from the end of the Cretaceous and, throughout the Palaeocene, the displacement between the African and European plates was clearly convergent and part of the future Internal Zone of the Betic Cordillera was affected. To the west, the Atlantic continued to open as a passive margin and, to the north, no significant deformation occurred. During the Eocene, the entire Iberian plate was subjected to compression. which caused major deformations in the Pyrenees and also in the Alpujarride and Nevado-Filabride, Internal Betic, complexes. In the Oligocene continued this situation, but in addition, the new extensional process ocurring in the western Mediterranean area, together with the constant eastward drift of Iberia due to Atlantic opening, compressed the eastern sector of Iberia, giving rise to the structuring of the Iberian Cordillera. The Neogene was the time when the Betic Cordillera reached its fundamental features with the westward displacement of the Betic-Rif Internal Zone, expelled by the progressive opening of the Algerian Basin, opening prolonged till the Alboran Sea. From the late Miocene onwards, all Iberia was affected by a N-S to NNW-SSE compression, combined in many points by a near perpendicular extension. Specially in eastern and southern Iberia a radial extension superposed these compression and extension. |
|---|---|
| Autores principais: | Galdeano, C. Sanz de |
| Assunto: | Iberia Betic Cordillera Cenozoic Western Mediterranean |
| Ano: | 2010 |
| País: | Portugal |
| Tipo de documento: | artigo |
| Tipo de acesso: | acesso aberto |
| Instituição associada: | Universidade Nova de Lisboa |
| Idioma: | inglês |
| Origem: | Repositório Institucional da UNL |
| _version_ | 1865920616531492864 |
|---|---|
| author | Galdeano, C. Sanz de |
| author_facet | Galdeano, C. Sanz de Galdeano, C. Sanz de |
| author_role | author |
| contributor_name_str_mv | RUN |
| country_str | PT |
| creators_json_str | [{\"Person.name\":\"Galdeano, C. Sanz de\"}] |
| datacite.contributors.contributor.contributorName.fl_str_mv | RUN |
| datacite.creators.creator.creatorName.fl_str_mv | Galdeano, C. Sanz de |
| datacite.date.Accepted.fl_str_mv | 2010-12-28T00:00:00Z |
| datacite.date.available.fl_str_mv | 2010-12-28T21:40:58Z |
| datacite.date.embargoed.fl_str_mv | 2010-12-28T21:40:58Z |
| datacite.rights.fl_str_mv | http://purl.org/coar/access_right/c_abf2 |
| datacite.subjects.subject.fl_str_mv | Iberia Betic Cordillera Cenozoic Western Mediterranean |
| datacite.titles.title.fl_str_mv | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| dc.contributor.none.fl_str_mv | RUN |
| dc.creator.none.fl_str_mv | Galdeano, C. Sanz de |
| dc.date.Accepted.fl_str_mv | 2010-12-28T00:00:00Z |
| dc.date.available.fl_str_mv | 2010-12-28T21:40:58Z |
| dc.date.embargoed.fl_str_mv | 2010-12-28T21:40:58Z |
| dc.format.none.fl_str_mv | application/pdf |
| dc.identifier.none.fl_str_mv | http://hdl.handle.net/10362/4695 |
| dc.language.none.fl_str_mv | eng |
| dc.rights.none.fl_str_mv | http://purl.org/coar/access_right/c_abf2 |
| dc.subject.none.fl_str_mv | Iberia Betic Cordillera Cenozoic Western Mediterranean |
| dc.title.fl_str_mv | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| dc.type.none.fl_str_mv | http://purl.org/coar/resource_type/c_6501 |
| description | The extensional process affecting Iberia during the Triassic and Jurassic times change from the end of the Cretaceous and, throughout the Palaeocene, the displacement between the African and European plates was clearly convergent and part of the future Internal Zone of the Betic Cordillera was affected. To the west, the Atlantic continued to open as a passive margin and, to the north, no significant deformation occurred. During the Eocene, the entire Iberian plate was subjected to compression. which caused major deformations in the Pyrenees and also in the Alpujarride and Nevado-Filabride, Internal Betic, complexes. In the Oligocene continued this situation, but in addition, the new extensional process ocurring in the western Mediterranean area, together with the constant eastward drift of Iberia due to Atlantic opening, compressed the eastern sector of Iberia, giving rise to the structuring of the Iberian Cordillera. The Neogene was the time when the Betic Cordillera reached its fundamental features with the westward displacement of the Betic-Rif Internal Zone, expelled by the progressive opening of the Algerian Basin, opening prolonged till the Alboran Sea. From the late Miocene onwards, all Iberia was affected by a N-S to NNW-SSE compression, combined in many points by a near perpendicular extension. Specially in eastern and southern Iberia a radial extension superposed these compression and extension. |
| dirty | 0 |
| eu_rights_str_mv | openAccess |
| format | article |
| fulltext.url.fl_str_mv | https://run.unl.pt/bitstreams/7bd9353d-a69a-48e7-92a0-fd24d949a98a/download |
| id | run_746cb324db366628b747bf7bfe9d1bbf |
| identifier.url.fl_str_mv | http://hdl.handle.net/10362/4695 |
| instacron_str | unl |
| institution | Universidade Nova de Lisboa |
| instname_str | Universidade Nova de Lisboa |
| language | eng |
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| network_name_str | Repositório Institucional da UNL |
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| organization_str_mv | urn:organizationAcronym:unl |
| person_str_mv | Galdeano, C. Sanz de |
| publishDate | 2010 |
| reponame_str | Repositório Institucional da UNL |
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| spelling | engen_USThe extensional process affecting Iberia during the Triassic and Jurassic times change from the end of the Cretaceous and, throughout the Palaeocene, the displacement between the African and European plates was clearly convergent and part of the future Internal Zone of the Betic Cordillera was affected. To the west, the Atlantic continued to open as a passive margin and, to the north, no significant deformation occurred. During the Eocene, the entire Iberian plate was subjected to compression. which caused major deformations in the Pyrenees and also in the Alpujarride and Nevado-Filabride, Internal Betic, complexes. In the Oligocene continued this situation, but in addition, the new extensional process ocurring in the western Mediterranean area, together with the constant eastward drift of Iberia due to Atlantic opening, compressed the eastern sector of Iberia, giving rise to the structuring of the Iberian Cordillera. The Neogene was the time when the Betic Cordillera reached its fundamental features with the westward displacement of the Betic-Rif Internal Zone, expelled by the progressive opening of the Algerian Basin, opening prolonged till the Alboran Sea. From the late Miocene onwards, all Iberia was affected by a N-S to NNW-SSE compression, combined in many points by a near perpendicular extension. Specially in eastern and southern Iberia a radial extension superposed these compression and extension.application/pdfen_USEvolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western MediterraneanGaldeano, C. Sanz deHostingInstitutionOrganizationalRUNe-mailmailto:run@unl.ptrun@unl.pt2010-12-28T21:40:58Z2010-12-282010-12-28T00:00:00ZHandlehttp://hdl.handle.net/10362/4695http://purl.org/coar/access_right/c_abf2open accessIberiaBetic CordilleraCenozoicWestern Mediterranean3303361 bytesliteraturehttp://purl.org/coar/resource_type/c_6501journal articlehttp://purl.org/coar/access_right/c_abf2application/pdffulltexthttps://run.unl.pt/bitstreams/7bd9353d-a69a-48e7-92a0-fd24d949a98a/download |
| spellingShingle | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean Galdeano, C. Sanz de Iberia Betic Cordillera Cenozoic Western Mediterranean Galdeano, C. Sanz de Iberia Betic Cordillera Cenozoic Western Mediterranean |
| status | NEW |
| subject.fl_str_mv | Iberia Betic Cordillera Cenozoic Western Mediterranean |
| title | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| title_full | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| title_fullStr | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| title_full_unstemmed | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| title_short | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| title_sort | Evolution of Iberia during the Cenozoic with special emphasis on the formation of the Betic Cordillera and its relation with the western Mediterranean |
| topic | Iberia Betic Cordillera Cenozoic Western Mediterranean |
| topic_facet | Iberia Betic Cordillera Cenozoic Western Mediterranean |
| url | http://hdl.handle.net/10362/4695 |
| visible | 1 |