Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results

Direct dating of reactivation of the San Jerónimo Fault (SJF), easternmost limit of the Romeral fault system (RFS), is presented through 39Ar-40Ar and K-Ar results in neo-formed micas and mylonitic bands of strongly hidrothermalized gabbros. Published cooling and crystallization ages from sin-tecton...

Full description

Autores:
Vinasco Vallejo, Cesar Javier
Cordani, Umberto
Tipo de recurso:
Article of journal
Fecha de publicación:
2012
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/71050
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/71050
http://bdigital.unal.edu.co/35520/
Palabra clave:
Romeral
Ar-Ar
Quebadagrande
Arquía
Central Cordillera
Colombia
Caribe
Plateau
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
id UNACIONAL2_7a7cac48875464605da0fd8a8b4f3d36
oai_identifier_str oai:repositorio.unal.edu.co:unal/71050
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
title Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
spellingShingle Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
Romeral
Ar-Ar
Quebadagrande
Arquía
Central Cordillera
Colombia
Caribe
Plateau
title_short Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
title_full Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
title_fullStr Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
title_full_unstemmed Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
title_sort Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results
dc.creator.fl_str_mv Vinasco Vallejo, Cesar Javier
Cordani, Umberto
dc.contributor.author.spa.fl_str_mv Vinasco Vallejo, Cesar Javier
Cordani, Umberto
dc.subject.proposal.spa.fl_str_mv Romeral
Ar-Ar
Quebadagrande
Arquía
Central Cordillera
Colombia
Caribe
Plateau
topic Romeral
Ar-Ar
Quebadagrande
Arquía
Central Cordillera
Colombia
Caribe
Plateau
description Direct dating of reactivation of the San Jerónimo Fault (SJF), easternmost limit of the Romeral fault system (RFS), is presented through 39Ar-40Ar and K-Ar results in neo-formed micas and mylonitic bands of strongly hidrothermalized gabbros. Published cooling and crystallization ages from sin-tectonic magmatic rocks exposed in the western fl ank of the Central Cordillera have suggest that tectonic evolution of the paleo-fault system began since Triassic and Lower Jurassic before the installation of Central Cordillera in its present position relative to the South American margin (SOAM). The Sabaletas greenchists (Arquía complex) yields 39Ar-40Ar plateau age of 127±5 Ma and integrated ages between 102-115 Ma eventually recording the initial accommodation of the Albian-Aptian volcanosedimentary sequence of the Quebradagrande Complex to the continental margin. Direct dating of fault reactivation of SJF through 39Ar-40Ar analysis in neo-formed micas in mylonitic bands and K-Ar ages in a hidrothermalized gabbro belonging to the Quebradagrande volcanic rocks shows plateau ages ranging from 87-90 Ma in biotite and 72-81 Ma in sericite, whereas K-Ar whole rock ages in samples collected in the area of infl uence of the SJF range between 91-102 Ma. The predominance of Upper Cretaceous ages suggest that activity of the fault system rich the major and most important peak during this time spam. This age interval is most likely related to the oblique arrival and collision of the Caribbean-Colombian Oceanic Plateau (CCOP) episodically during the upper cretaceous. Final deformational episodes in the Central Cordillera and RFS are related to the collision of the Panamá-Chocó block in Early Mioceneearly Pliocene, and are recorded by 39Ar-40Ar and K-Ar ages in Mio-Pliocene intrusives along the Cauca depression.
publishDate 2012
dc.date.issued.spa.fl_str_mv 2012
dc.date.accessioned.spa.fl_str_mv 2019-07-03T14:14:51Z
dc.date.available.spa.fl_str_mv 2019-07-03T14:14:51Z
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/71050
dc.identifier.eprints.spa.fl_str_mv http://bdigital.unal.edu.co/35520/
url https://repositorio.unal.edu.co/handle/unal/71050
http://bdigital.unal.edu.co/35520/
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/35877
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. 32 (2012); 111-124 0120-3630
dc.relation.references.spa.fl_str_mv Vinasco Vallejo, Cesar Javier and Cordani, Umberto (2012) Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results. Boletín Ciencias de la Tierra; núm. 32 (2012); 111-124 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 https://repositorio.unal.edu.co/bitstream/unal/71050/1/35877-144528-1-SP.jpg
https://repositorio.unal.edu.co/bitstream/unal/71050/2/35877-189842-1-PB.html
https://repositorio.unal.edu.co/bitstream/unal/71050/3/35877-144532-1-SP.jpg
https://repositorio.unal.edu.co/bitstream/unal/71050/4/35877-144529-1-SP.jpg
https://repositorio.unal.edu.co/bitstream/unal/71050/5/35877-144530-1-SP.jpg
https://repositorio.unal.edu.co/bitstream/unal/71050/6/35877-144547-1-SP.docx
https://repositorio.unal.edu.co/bitstream/unal/71050/7/35877-144531-1-SP.jpg
https://repositorio.unal.edu.co/bitstream/unal/71050/8/35877-161230-1-PB.pdf
https://repositorio.unal.edu.co/bitstream/unal/71050/9/35877-161230-1-PB.pdf.jpg
bitstream.checksum.fl_str_mv f7d364be8c6300f3996c3c19bc967c0b
87179194b538a412fac9c6452d1b0506
4bb1b360c3920efcc2d6a621098a8987
6a40efc03b26c8d5540068ce49bc5a5c
d408c338653b19eb6a2c492614f0f725
1ca43ca4aa876e7413fb47108b360202
b83c22870f0293e8f256ea1396900077
06499fa6136ce7307b534c70c5ea5422
a15486c8605f873823ce5a1a9af00643
bitstream.checksumAlgorithm.fl_str_mv MD5
MD5
MD5
MD5
MD5
MD5
MD5
MD5
MD5
repository.name.fl_str_mv Repositorio Institucional Universidad Nacional de Colombia
repository.mail.fl_str_mv repositorio_nal@unal.edu.co
_version_ 1806886191778234368
spelling 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_abf2Vinasco Vallejo, Cesar Javier49b3ca42-f249-4f4a-9d86-bb6ba7c93069300Cordani, Umberto18bb8a56-ce5b-44d5-a6b4-604f4e1984613002019-07-03T14:14:51Z2019-07-03T14:14:51Z2012https://repositorio.unal.edu.co/handle/unal/71050http://bdigital.unal.edu.co/35520/Direct dating of reactivation of the San Jerónimo Fault (SJF), easternmost limit of the Romeral fault system (RFS), is presented through 39Ar-40Ar and K-Ar results in neo-formed micas and mylonitic bands of strongly hidrothermalized gabbros. Published cooling and crystallization ages from sin-tectonic magmatic rocks exposed in the western fl ank of the Central Cordillera have suggest that tectonic evolution of the paleo-fault system began since Triassic and Lower Jurassic before the installation of Central Cordillera in its present position relative to the South American margin (SOAM). The Sabaletas greenchists (Arquía complex) yields 39Ar-40Ar plateau age of 127±5 Ma and integrated ages between 102-115 Ma eventually recording the initial accommodation of the Albian-Aptian volcanosedimentary sequence of the Quebradagrande Complex to the continental margin. Direct dating of fault reactivation of SJF through 39Ar-40Ar analysis in neo-formed micas in mylonitic bands and K-Ar ages in a hidrothermalized gabbro belonging to the Quebradagrande volcanic rocks shows plateau ages ranging from 87-90 Ma in biotite and 72-81 Ma in sericite, whereas K-Ar whole rock ages in samples collected in the area of infl uence of the SJF range between 91-102 Ma. The predominance of Upper Cretaceous ages suggest that activity of the fault system rich the major and most important peak during this time spam. This age interval is most likely related to the oblique arrival and collision of the Caribbean-Colombian Oceanic Plateau (CCOP) episodically during the upper cretaceous. Final deformational episodes in the Central Cordillera and RFS are related to the collision of the Panamá-Chocó block in Early Mioceneearly Pliocene, and are recorded by 39Ar-40Ar and K-Ar ages in Mio-Pliocene intrusives along the Cauca depression.application/pdfspaUniversidad Nacional de Colombiahttp://revistas.unal.edu.co/index.php/rbct/article/view/35877Universidad Nacional de Colombia Revistas electrónicas UN Boletín Ciencias de la TierraBoletín Ciencias de la TierraBoletín Ciencias de la Tierra; núm. 32 (2012); 111-124 0120-3630Vinasco Vallejo, Cesar Javier and Cordani, Umberto (2012) Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar results. Boletín Ciencias de la Tierra; núm. 32 (2012); 111-124 0120-3630 .Reactivation episodes of the romeral fault system in the northwestern part of central andes, colombia, through 39ar-40ar and k-ar resultsArtículo 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/ARTRomeralAr-ArQuebadagrandeArquíaCentral CordilleraColombiaCaribePlateauORIGINAL35877-144528-1-SP.jpgimage/jpeg347361https://repositorio.unal.edu.co/bitstream/unal/71050/1/35877-144528-1-SP.jpgf7d364be8c6300f3996c3c19bc967c0bMD5135877-189842-1-PB.htmltext/html49640https://repositorio.unal.edu.co/bitstream/unal/71050/2/35877-189842-1-PB.html87179194b538a412fac9c6452d1b0506MD5235877-144532-1-SP.jpgimage/jpeg425514https://repositorio.unal.edu.co/bitstream/unal/71050/3/35877-144532-1-SP.jpg4bb1b360c3920efcc2d6a621098a8987MD5335877-144529-1-SP.jpgimage/jpeg635736https://repositorio.unal.edu.co/bitstream/unal/71050/4/35877-144529-1-SP.jpg6a40efc03b26c8d5540068ce49bc5a5cMD5435877-144530-1-SP.jpgimage/jpeg346754https://repositorio.unal.edu.co/bitstream/unal/71050/5/35877-144530-1-SP.jpgd408c338653b19eb6a2c492614f0f725MD5535877-144547-1-SP.docxapplication/vnd.openxmlformats-officedocument.wordprocessingml.document42329https://repositorio.unal.edu.co/bitstream/unal/71050/6/35877-144547-1-SP.docx1ca43ca4aa876e7413fb47108b360202MD5635877-144531-1-SP.jpgimage/jpeg265678https://repositorio.unal.edu.co/bitstream/unal/71050/7/35877-144531-1-SP.jpgb83c22870f0293e8f256ea1396900077MD5735877-161230-1-PB.pdfapplication/pdf729242https://repositorio.unal.edu.co/bitstream/unal/71050/8/35877-161230-1-PB.pdf06499fa6136ce7307b534c70c5ea5422MD58THUMBNAIL35877-161230-1-PB.pdf.jpg35877-161230-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg9443https://repositorio.unal.edu.co/bitstream/unal/71050/9/35877-161230-1-PB.pdf.jpga15486c8605f873823ce5a1a9af00643MD59unal/71050oai:repositorio.unal.edu.co:unal/710502023-06-16 23:03:52.449Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co