The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)

The Middle Triassic in the NW of the Iberian Basin consists of both carbonate and terrigenous sediments. A new sedimentary model is proposed for the clastic wedge of the Cuesta del Castillo Saudstones and Siltstones (CCSS) Formation (García-Gil, 1990), and its relationship with the Upper Muschelkalk...

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Bibliographic Details
Author: García Gil, S.
Format: article
Publication Date:1991
Country:España
Institution:Universidad Complutense de Madrid (UCM)
Repository:Docta Complutense
Language:English
OAI Identifier:oai:docta.ucm.es:20.500.14352/58038
Online Access:https://hdl.handle.net/20.500.14352/58038
Access Level:Open access
Keyword:551.3.051(234.1)
Iberian Rasiges
Triassic
Muschellcallc
Homoclinal ramp
Alluvial delta
Continental facies
Shallow marines facies
Terrigenous
Depositional sequences
Cordillera Ibérica
Triásico
Muschelkalk
Rampa itomoclinal
Delta aluvial
Facies continentales
Facies marinas someras
Terrígenos
Secuencias deposicionales
Geología estratigráfica
2506.19 Estratigrafía
id ES_3c3ba48555ced848c8d2f7d44d2d39b4
oai_identifier_str oai:docta.ucm.es:20.500.14352/58038
network_acronym_str ES
network_name_str España
repository_id_str
spelling The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)García Gil, S.551.3.051(234.1)Iberian RasigesTriassicMuschellcallcHomoclinal rampAlluvial deltaContinental faciesShallow marines faciesTerrigenousDepositional sequencesCordillera IbéricaTriásicoMuschelkalkRampa itomoclinalDelta aluvialFacies continentalesFacies marinas somerasTerrígenosSecuencias deposicionalesGeología estratigráfica2506.19 EstratigrafíaThe Middle Triassic in the NW of the Iberian Basin consists of both carbonate and terrigenous sediments. A new sedimentary model is proposed for the clastic wedge of the Cuesta del Castillo Saudstones and Siltstones (CCSS) Formation (García-Gil, 1990), and its relationship with the Upper Muschelkalk carbonate Formations. The model will take account of tite following characteristics: 1. Low depositional gradient being integrated in a homoclinal carbonate ramp. 2. Combined tectonic, climatic aud eustatic controis. 3. Presence of continental antA shallow marine facies associations. 4. Homogeneity of textural facies. The sedimentation of tite CCSS Formation took place during a relative sea level rise (high stand system tract).Editorial ComplutenseUniversidad Complutense de Madrid19911991-01-0119911991-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/20.500.14352/58038reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/580382026-06-02T12:44:21Z
dc.title.none.fl_str_mv The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
title The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
spellingShingle The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
García Gil, S.
551.3.051(234.1)
Iberian Rasiges
Triassic
Muschellcallc
Homoclinal ramp
Alluvial delta
Continental facies
Shallow marines facies
Terrigenous
Depositional sequences
Cordillera Ibérica
Triásico
Muschelkalk
Rampa itomoclinal
Delta aluvial
Facies continentales
Facies marinas someras
Terrígenos
Secuencias deposicionales
Geología estratigráfica
2506.19 Estratigrafía
title_short The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
title_full The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
title_fullStr The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
title_full_unstemmed The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
title_sort The sedimentological significance of a clastic wedge in the western basin margin of the Triassic Tethys (Iberian Range, Spain)
dc.creator.none.fl_str_mv García Gil, S.
author García Gil, S.
author_facet García Gil, S.
author_role author
dc.contributor.none.fl_str_mv Universidad Complutense de Madrid
dc.subject.none.fl_str_mv 551.3.051(234.1)
Iberian Rasiges
Triassic
Muschellcallc
Homoclinal ramp
Alluvial delta
Continental facies
Shallow marines facies
Terrigenous
Depositional sequences
Cordillera Ibérica
Triásico
Muschelkalk
Rampa itomoclinal
Delta aluvial
Facies continentales
Facies marinas someras
Terrígenos
Secuencias deposicionales
Geología estratigráfica
2506.19 Estratigrafía
topic 551.3.051(234.1)
Iberian Rasiges
Triassic
Muschellcallc
Homoclinal ramp
Alluvial delta
Continental facies
Shallow marines facies
Terrigenous
Depositional sequences
Cordillera Ibérica
Triásico
Muschelkalk
Rampa itomoclinal
Delta aluvial
Facies continentales
Facies marinas someras
Terrígenos
Secuencias deposicionales
Geología estratigráfica
2506.19 Estratigrafía
description The Middle Triassic in the NW of the Iberian Basin consists of both carbonate and terrigenous sediments. A new sedimentary model is proposed for the clastic wedge of the Cuesta del Castillo Saudstones and Siltstones (CCSS) Formation (García-Gil, 1990), and its relationship with the Upper Muschelkalk carbonate Formations. The model will take account of tite following characteristics: 1. Low depositional gradient being integrated in a homoclinal carbonate ramp. 2. Combined tectonic, climatic aud eustatic controis. 3. Presence of continental antA shallow marine facies associations. 4. Homogeneity of textural facies. The sedimentation of tite CCSS Formation took place during a relative sea level rise (high stand system tract).
publishDate 1991
dc.date.none.fl_str_mv 1991
1991-01-01
1991
1991-01-01
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/20.500.14352/58038
url https://hdl.handle.net/20.500.14352/58038
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
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 Editorial Complutense
publisher.none.fl_str_mv Editorial Complutense
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_ 1869406356606287872
score 15.300724

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