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...
- 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
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|
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 |
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application/pdf |
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Universidad Nacional de Colombia |
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Universidad Nacional de Colombia |
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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_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 |