A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes
Metamorphic pressure and temperature trajectories are generally used as tools to interpret the tectonic history ofdeformed belts of rocks that record past activity along active plate margins. The pre-Devonian metamorphic sequenceof the Silgará Formation forms part of the ancient basement of the cent...
- Autores:
-
Castellanos A., Óscar M.
Ríos R, Carlos A
Takasu, Akira
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2008
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/33993
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/33993
http://bdigital.unal.edu.co/24073/
- Palabra clave:
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
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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_abf2Castellanos A., Óscar M.38199641-6191-404a-9295-874871210058300Ríos R, Carlos A0cead47d-2f80-4923-8bb6-17aebde6d70f300Takasu, Akirac6071a25-c6b8-4ad9-81ed-6943bbd18e703002019-06-27T23:09:14Z2019-06-27T23:09:14Z2008https://repositorio.unal.edu.co/handle/unal/33993http://bdigital.unal.edu.co/24073/Metamorphic pressure and temperature trajectories are generally used as tools to interpret the tectonic history ofdeformed belts of rocks that record past activity along active plate margins. The pre-Devonian metamorphic sequenceof the Silgará Formation forms part of the ancient basement of the central Santander Massif, including pelitic schists, siliceous schists and intercalation of amphibolites accompanied by marble. This metasedimentary unit has been affected by Barrovian type metamorphism under middle-pressure/high-temperature conditions. This paper presents on the relationship of tectonic processes to pressure-temperature paths development.Detailed petrologic analysis of pelites and related rocks has been used to constrain the P-T history of this region in the eastern colombian cordillera. Mineral assemblages and Geothermobarometric calculations indicate metamorphic temperatures and pressures of 400-600 °C and 4.0-6.5 kbar, respectively.application/pdfspaUNIVERSIDAD NACIONAL DE COLOMBIAhttp://revistas.unal.edu.co/index.php/esrj/article/view/21185Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalEarth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 2339-3459 1794-6190Castellanos A., Óscar M. and Ríos R, Carlos A and Takasu, Akira (2008) A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes. Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 2339-3459 1794-6190 .A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andesArtículo 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/ARTORIGINAL21185-71888-1-PB.pdfapplication/pdf2249935https://repositorio.unal.edu.co/bitstream/unal/33993/1/21185-71888-1-PB.pdf1097220b74d9a4a874cbebb790afa5e4MD51THUMBNAIL21185-71888-1-PB.pdf.jpg21185-71888-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg6463https://repositorio.unal.edu.co/bitstream/unal/33993/2/21185-71888-1-PB.pdf.jpg91479bf5c327892797bf1f11233ec1e0MD52unal/33993oai:repositorio.unal.edu.co:unal/339932023-12-24 23:05:29.456Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |
dc.title.spa.fl_str_mv |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
title |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
spellingShingle |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
title_short |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
title_full |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
title_fullStr |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
title_full_unstemmed |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
title_sort |
A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes |
dc.creator.fl_str_mv |
Castellanos A., Óscar M. Ríos R, Carlos A Takasu, Akira |
dc.contributor.author.spa.fl_str_mv |
Castellanos A., Óscar M. Ríos R, Carlos A Takasu, Akira |
description |
Metamorphic pressure and temperature trajectories are generally used as tools to interpret the tectonic history ofdeformed belts of rocks that record past activity along active plate margins. The pre-Devonian metamorphic sequenceof the Silgará Formation forms part of the ancient basement of the central Santander Massif, including pelitic schists, siliceous schists and intercalation of amphibolites accompanied by marble. This metasedimentary unit has been affected by Barrovian type metamorphism under middle-pressure/high-temperature conditions. This paper presents on the relationship of tectonic processes to pressure-temperature paths development.Detailed petrologic analysis of pelites and related rocks has been used to constrain the P-T history of this region in the eastern colombian cordillera. Mineral assemblages and Geothermobarometric calculations indicate metamorphic temperatures and pressures of 400-600 °C and 4.0-6.5 kbar, respectively. |
publishDate |
2008 |
dc.date.issued.spa.fl_str_mv |
2008 |
dc.date.accessioned.spa.fl_str_mv |
2019-06-27T23:09:14Z |
dc.date.available.spa.fl_str_mv |
2019-06-27T23:09:14Z |
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/33993 |
dc.identifier.eprints.spa.fl_str_mv |
http://bdigital.unal.edu.co/24073/ |
url |
https://repositorio.unal.edu.co/handle/unal/33993 http://bdigital.unal.edu.co/24073/ |
dc.language.iso.spa.fl_str_mv |
spa |
language |
spa |
dc.relation.spa.fl_str_mv |
http://revistas.unal.edu.co/index.php/esrj/article/view/21185 |
dc.relation.ispartof.spa.fl_str_mv |
Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal Earth Sciences Research Journal |
dc.relation.ispartofseries.none.fl_str_mv |
Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 2339-3459 1794-6190 |
dc.relation.references.spa.fl_str_mv |
Castellanos A., Óscar M. and Ríos R, Carlos A and Takasu, Akira (2008) A new approach on the tectonometamorphic mechanisms associated with p–t paths of the barrovian-type silgará formation at the central santander massif, colombian andes. Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 Earth Sciences Research Journal; Vol. 12, núm. 2 (2008); 125-155 2339-3459 1794-6190 . |
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 |
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UNIVERSIDAD NACIONAL DE COLOMBIA |
institution |
Universidad Nacional de Colombia |
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