Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics

Analyses of composition and sedimentological attributes of conglomerate clasts together with petrographical and heavy mineral analyses and detrital geochronology from sandstones of the Oligocene Siamaná Formation in the Serranía de Jarara, are presented in order to reconstruct de provenance of this...

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Autores:
Zapata, Sebastián
Weber Scharff, Marión Beatriz I
Cardona, Agustín
Valencia, Víctor
Guzmán Ospitia, Georgina
Tobón, Mónica
Tipo de recurso:
Article of journal
Fecha de publicación:
2010
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/30740
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/30740
http://bdigital.unal.edu.co/20816/
Palabra clave:
Colombia
Guajira
Caribbean plate
Oligocene
pullapart basin
provenance
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
id UNACIONAL2_f96bbe7a3a40bc5bbde5388293f49bed
oai_identifier_str oai:repositorio.unal.edu.co:unal/30740
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
title Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
spellingShingle Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
Colombia
Guajira
Caribbean plate
Oligocene
pullapart basin
provenance
title_short Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
title_full Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
title_fullStr Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
title_full_unstemmed Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
title_sort Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics
dc.creator.fl_str_mv Zapata, Sebastián
Weber Scharff, Marión Beatriz I
Cardona, Agustín
Valencia, Víctor
Guzmán Ospitia, Georgina
Tobón, Mónica
dc.contributor.author.spa.fl_str_mv Zapata, Sebastián
Weber Scharff, Marión Beatriz I
Cardona, Agustín
Valencia, Víctor
Guzmán Ospitia, Georgina
Tobón, Mónica
dc.subject.proposal.spa.fl_str_mv Colombia
Guajira
Caribbean plate
Oligocene
pullapart basin
provenance
topic Colombia
Guajira
Caribbean plate
Oligocene
pullapart basin
provenance
description Analyses of composition and sedimentological attributes of conglomerate clasts together with petrographical and heavy mineral analyses and detrital geochronology from sandstones of the Oligocene Siamaná Formation in the Serranía de Jarara, are presented in order to reconstruct de provenance of this sedimentary sequence and contribute to the knowledge of the tectonosedimentary evolution of the Guajira Peninsula and the Caribbean. The results indicate that the source areas are proximal and are located to the southeast. The presence of plutonic igneous and mediumto Lowgrade metamorphic rocks, as well as highpressure metamorphic rocks, indicate that the lithostratigraphic units (Parashi Stock and Jarara Formation) of the Serranía de Jarara and an unidentified unit to the southeast, are the main rock sources. The heavy minerals and the detrital zircon distribution with peaks at approximately 50 Ma, 207Ma, 245 Ma, 463 Ma, 963 Ma and 1044 Ma, confirm that this is the source area. The extremely proximate sources and the rapid burying of the basin, which is evident due to the presence of marine sediments that overlie this sequence, indicate that this siliciclastic unit is related to the initial phases of a pullapart basin. This basin was probably formed as a result of the movement of the Caribbean plate towards the east. The origin of the highpressure clasts is unknown, and is possibly linked to a tectonic mélange. The U-Pb ages of approximately 50 Ma and the presence of fragments from the Parashi Stock, suggest exhumation during the Eocene and Upper Oligocene, possibly linked to the formation of the basin.
publishDate 2010
dc.date.issued.spa.fl_str_mv 2010
dc.date.accessioned.spa.fl_str_mv 2019-06-26T14:12:16Z
dc.date.available.spa.fl_str_mv 2019-06-26T14:12:16Z
dc.type.spa.fl_str_mv Artículo de revista
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dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
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url https://repositorio.unal.edu.co/handle/unal/30740
http://bdigital.unal.edu.co/20816/
dc.language.iso.spa.fl_str_mv spa
language spa
dc.relation.spa.fl_str_mv http://revistas.unal.edu.co/index.php/rbct/article/view/17045
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Boletín Ciencias de la Tierra
Boletín Ciencias de la Tierra
dc.relation.ispartofseries.none.fl_str_mv Boletín Ciencias de la Tierra; núm. 27 (2010); 07-24 0120-3630
dc.relation.references.spa.fl_str_mv Zapata, Sebastián and Weber Scharff, Marión Beatriz I and Cardona, Agustín and Valencia, Víctor and Guzmán Ospitia, Georgina and Tobón, Mónica (2010) Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonics. Boletín Ciencias de la Tierra; núm. 27 (2010); 07-24 0120-3630 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
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dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
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dc.publisher.spa.fl_str_mv Universidad Nacional de Colombia
institution Universidad Nacional de Colombia
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