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...
- 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
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|
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 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.content.spa.fl_str_mv |
Text |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/ART |
format |
http://purl.org/coar/resource_type/c_6501 |
status_str |
publishedVersion |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/30740 |
dc.identifier.eprints.spa.fl_str_mv |
http://bdigital.unal.edu.co/20816/ |
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 |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.license.spa.fl_str_mv |
Atribución-NoComercial 4.0 Internacional |
dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/licenses/by-nc/4.0/ |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Atribución-NoComercial 4.0 Internacional Derechos reservados - Universidad Nacional de Colombia http://creativecommons.org/licenses/by-nc/4.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
dc.format.mimetype.spa.fl_str_mv |
application/pdf |
dc.publisher.spa.fl_str_mv |
Universidad Nacional de Colombia |
institution |
Universidad Nacional de Colombia |
bitstream.url.fl_str_mv |
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Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Zapata, Sebastián6d54e5aa-8de1-40ed-b1f4-60036cb4ed82300Weber Scharff, Marión Beatriz Ic1565fb5-7bda-4afe-9126-5c8f14022747300Cardona, Agustíne46f4217-eeae-4d08-b4a7-27eab1d70095300Valencia, Víctor48bd0208-b4ad-44a8-b794-fecb1fdf3eed300Guzmán Ospitia, Georgina72f7298f-7d2e-4d32-ac9b-b4bebc515cb6300Tobón, Mónicab30a6edc-2608-4702-9a46-0784bc1ff5aa3002019-06-26T14:12:16Z2019-06-26T14:12:16Z2010https://repositorio.unal.edu.co/handle/unal/30740http://bdigital.unal.edu.co/20816/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.application/pdfspaUniversidad Nacional de Colombiahttp://revistas.unal.edu.co/index.php/rbct/article/view/17045Universidad Nacional de Colombia Revistas electrónicas UN Boletín Ciencias de la TierraBoletín Ciencias de la TierraBoletín Ciencias de la Tierra; núm. 27 (2010); 07-24 0120-3630Zapata, 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 .Provenance of oligocene conglomerates and associated sandstones from the siamanáformation, serraníade jarara, guajira, colombia: implications for oligocene caribbean-south american tectonicsArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTColombiaGuajiraCaribbean plateOligocenepullapart basinprovenanceORIGINAL17045-53874-1-PB.htmtext/html45107https://repositorio.unal.edu.co/bitstream/unal/30740/1/17045-53874-1-PB.htm52469da40a9bcadad656bb9cf22660b0MD5117045-53873-1-PB.pdfapplication/pdf3618276https://repositorio.unal.edu.co/bitstream/unal/30740/2/17045-53873-1-PB.pdf58d5a361fa7b5d5cfccd0ec536327e7aMD52THUMBNAIL17045-53873-1-PB.pdf.jpg17045-53873-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg9792https://repositorio.unal.edu.co/bitstream/unal/30740/3/17045-53873-1-PB.pdf.jpg571d9b1f92a277a2e29e4f8b3d5631e1MD53unal/30740oai:repositorio.unal.edu.co:unal/307402023-11-26 23:05:31.626Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |