Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico
The Cehegín Formation (Ladinian) is defined as a formal lithostratigraphic unit to characterize the Muschelkalk facies deposited on intermediate-external area of the southern Iberian continental margin. This formation consists of dark limestones and marly limestones. Two main members can be distingu...
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2005 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/52494 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/52494 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.7 Muschelkalk Triassic Lithostratigraphic unit Betic Cordillera Epicontinental Geología estratigráfica 2506.19 Estratigrafía |
| id |
ES_4f4d98270cc7efbddada2e2ca08c2deb |
|---|---|
| oai_identifier_str |
oai:docta.ucm.es:20.500.14352/52494 |
| network_acronym_str |
ES |
| network_name_str |
España |
| repository_id_str |
|
| spelling |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen SudibéricoPérez Valera, FernandoPérez López, A.Pérez Valera, J. Alberto551.7MuschelkalkTriassicLithostratigraphic unitBetic CordilleraEpicontinentalGeología estratigráfica2506.19 EstratigrafíaThe Cehegín Formation (Ladinian) is defined as a formal lithostratigraphic unit to characterize the Muschelkalk facies deposited on intermediate-external area of the southern Iberian continental margin. This formation consists of dark limestones and marly limestones. Two main members can be distinguished in this formation. In the lower member, two o three massive carbonate thick beds appear with bedded marly limestone intercalations. The upper member consists of a more marly succession of carbonate beds with burrows and intercalations of bioclastic limestone. Pot and gutter casts are frequent in the lower member, and tempestites occur mainly in the upper member. The sediments of this formations are interpreted as epicontinental marine deposits. The holostratotype, parastratotypes and hypostratotype which characterize this formation in the Betic Cordillera are described.Sociedad Geológica de EspañaUniversidad Complutense de Madrid20052005-01-0120052005-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/20.500.14352/52494reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/524942026-06-02T12:44:21Z |
| dc.title.none.fl_str_mv |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| title |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| spellingShingle |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico Pérez Valera, Fernando 551.7 Muschelkalk Triassic Lithostratigraphic unit Betic Cordillera Epicontinental Geología estratigráfica 2506.19 Estratigrafía |
| title_short |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| title_full |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| title_fullStr |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| title_full_unstemmed |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| title_sort |
Definición de la Formación Cehegín para los carbonatos de faciès Muschelkalk depositados en un área intermedia-externa del Paleomargen Sudibérico |
| dc.creator.none.fl_str_mv |
Pérez Valera, Fernando Pérez López, A. Pérez Valera, J. Alberto |
| author |
Pérez Valera, Fernando |
| author_facet |
Pérez Valera, Fernando Pérez López, A. Pérez Valera, J. Alberto |
| author_role |
author |
| author2 |
Pérez López, A. Pérez Valera, J. Alberto |
| author2_role |
author author |
| dc.contributor.none.fl_str_mv |
Universidad Complutense de Madrid |
| dc.subject.none.fl_str_mv |
551.7 Muschelkalk Triassic Lithostratigraphic unit Betic Cordillera Epicontinental Geología estratigráfica 2506.19 Estratigrafía |
| topic |
551.7 Muschelkalk Triassic Lithostratigraphic unit Betic Cordillera Epicontinental Geología estratigráfica 2506.19 Estratigrafía |
| description |
The Cehegín Formation (Ladinian) is defined as a formal lithostratigraphic unit to characterize the Muschelkalk facies deposited on intermediate-external area of the southern Iberian continental margin. This formation consists of dark limestones and marly limestones. Two main members can be distinguished in this formation. In the lower member, two o three massive carbonate thick beds appear with bedded marly limestone intercalations. The upper member consists of a more marly succession of carbonate beds with burrows and intercalations of bioclastic limestone. Pot and gutter casts are frequent in the lower member, and tempestites occur mainly in the upper member. The sediments of this formations are interpreted as epicontinental marine deposits. The holostratotype, parastratotypes and hypostratotype which characterize this formation in the Betic Cordillera are described. |
| publishDate |
2005 |
| dc.date.none.fl_str_mv |
2005 2005-01-01 2005 2005-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/20.500.14352/52494 |
| url |
https://hdl.handle.net/20.500.14352/52494 |
| dc.language.none.fl_str_mv |
Español spa |
| language_invalid_str_mv |
Español |
| language |
spa |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
open access http://purl.org/coar/access_right/c_abf2 |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Sociedad Geológica de España |
| publisher.none.fl_str_mv |
Sociedad Geológica de España |
| dc.source.none.fl_str_mv |
reponame:Docta Complutense instname:Universidad Complutense de Madrid (UCM) |
| instname_str |
Universidad Complutense de Madrid (UCM) |
| reponame_str |
Docta Complutense |
| collection |
Docta Complutense |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
|
| _version_ |
1869407811715203072 |
| score |
15,300724 |