Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia
The Muzo, Tunja and Paipa lineaments are important Northwest-Southeast trending tectonic elements found in the Bogota-Sogamoso sector of the Eastern Cordillera of Colombia. They are superficially expressed as notorious aligments of topographic lows that exert a strong Influence on drainage as well a...
- Autores:
-
Ujueta L., Guillermo
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 1993
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/41878
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/41878
http://bdigital.unal.edu.co/31975/
- Palabra clave:
- Geología
Ciencias de la tierra
Geociencias
Elementos tectónicos
Cordillera Oriental
depresiones topográficas
pliegues
fallas
Geología
Ciencias de la tierra
Geociencias
Elementos tectónicos
Cordillera Oriental
depresiones topográficas
pliegues
fallas
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
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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_abf2Ujueta L., Guillermo11483135-158d-469d-b41d-9516bedebfe23002019-06-28T10:20:06Z2019-06-28T10:20:06Z1993https://repositorio.unal.edu.co/handle/unal/41878http://bdigital.unal.edu.co/31975/The Muzo, Tunja and Paipa lineaments are important Northwest-Southeast trending tectonic elements found in the Bogota-Sogamoso sector of the Eastern Cordillera of Colombia. They are superficially expressed as notorious aligments of topographic lows that exert a strong Influence on drainage as well as being directly related to the appearance and delimitation of the high plains found In this part of the cordillera. The best evidence towards the structural control exerted by these NW-SE structures is the rupture and displacement of those structures parallel to the general trend of the cordillera. Examples of these are the truncation or distortion of individual folds or faults or the displacement of groups of folds and faults. Several volcanic centers, lesser intrusions and high temperature hot springs are found along the proposed lineaments. In connection with the former, at aligned intervals are found mainly emerald occurrences as well as non-economic copper, iron, fluoride, lead and zinc deposits. Their occurrence is such that they may be directly related to the circulation of hydrothermal fluids that gave rise to such deposits. The nature of these reasonably parallel lineaments regularly spaced every 40 to 50 km, repeatedly reactivated and with lengths of hundreds of kilometers such as those here considered is important in the tectonic history not only of the Eastern Cordillera but also of the subandean basin of the Llanos Orientales and even of the Guayanan Craton itself.application/pdfspaDepartamento de Geocienciashttp://revistas.unal.edu.co/index.php/geocol/article/view/31302Universidad Nacional de Colombia Revistas electrónicas UN Geología ColombianaGeología ColombianaGeología Colombiana - An International Journal on Geosciences; Vol. 18 (1993); 65-73 Geología Colombiana; Vol. 18 (1993); 65-73 2357-3767 0072-0992Ujueta L., Guillermo (1993) Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia. Geología Colombiana - An International Journal on Geosciences; Vol. 18 (1993); 65-73 Geología Colombiana; Vol. 18 (1993); 65-73 2357-3767 0072-0992 .Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombiaArtículo 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/ARTGeologíaCiencias de la tierraGeocienciasElementos tectónicosCordillera Orientaldepresiones topográficasplieguesfallasGeologíaCiencias de la tierraGeocienciasElementos tectónicosCordillera Orientaldepresiones topográficasplieguesfallasORIGINAL31302-113377-1-PB.pdfapplication/pdf8052653https://repositorio.unal.edu.co/bitstream/unal/41878/1/31302-113377-1-PB.pdfbf9046ce6ec677ec430c9c457841015cMD51THUMBNAIL31302-113377-1-PB.pdf.jpg31302-113377-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg11911https://repositorio.unal.edu.co/bitstream/unal/41878/2/31302-113377-1-PB.pdf.jpg2b8beab1bd751e2e6ecd6c152dabb611MD52unal/41878oai:repositorio.unal.edu.co:unal/418782023-02-04 23:07:43.319Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |
dc.title.spa.fl_str_mv |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
title |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
spellingShingle |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia Geología Ciencias de la tierra Geociencias Elementos tectónicos Cordillera Oriental depresiones topográficas pliegues fallas Geología Ciencias de la tierra Geociencias Elementos tectónicos Cordillera Oriental depresiones topográficas pliegues fallas |
title_short |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
title_full |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
title_fullStr |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
title_full_unstemmed |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
title_sort |
Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia |
dc.creator.fl_str_mv |
Ujueta L., Guillermo |
dc.contributor.author.spa.fl_str_mv |
Ujueta L., Guillermo |
dc.subject.proposal.spa.fl_str_mv |
Geología Ciencias de la tierra Geociencias Elementos tectónicos Cordillera Oriental depresiones topográficas pliegues fallas Geología Ciencias de la tierra Geociencias Elementos tectónicos Cordillera Oriental depresiones topográficas pliegues fallas |
topic |
Geología Ciencias de la tierra Geociencias Elementos tectónicos Cordillera Oriental depresiones topográficas pliegues fallas Geología Ciencias de la tierra Geociencias Elementos tectónicos Cordillera Oriental depresiones topográficas pliegues fallas |
description |
The Muzo, Tunja and Paipa lineaments are important Northwest-Southeast trending tectonic elements found in the Bogota-Sogamoso sector of the Eastern Cordillera of Colombia. They are superficially expressed as notorious aligments of topographic lows that exert a strong Influence on drainage as well as being directly related to the appearance and delimitation of the high plains found In this part of the cordillera. The best evidence towards the structural control exerted by these NW-SE structures is the rupture and displacement of those structures parallel to the general trend of the cordillera. Examples of these are the truncation or distortion of individual folds or faults or the displacement of groups of folds and faults. Several volcanic centers, lesser intrusions and high temperature hot springs are found along the proposed lineaments. In connection with the former, at aligned intervals are found mainly emerald occurrences as well as non-economic copper, iron, fluoride, lead and zinc deposits. Their occurrence is such that they may be directly related to the circulation of hydrothermal fluids that gave rise to such deposits. The nature of these reasonably parallel lineaments regularly spaced every 40 to 50 km, repeatedly reactivated and with lengths of hundreds of kilometers such as those here considered is important in the tectonic history not only of the Eastern Cordillera but also of the subandean basin of the Llanos Orientales and even of the Guayanan Craton itself. |
publishDate |
1993 |
dc.date.issued.spa.fl_str_mv |
1993 |
dc.date.accessioned.spa.fl_str_mv |
2019-06-28T10:20:06Z |
dc.date.available.spa.fl_str_mv |
2019-06-28T10:20:06Z |
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/41878 |
dc.identifier.eprints.spa.fl_str_mv |
http://bdigital.unal.edu.co/31975/ |
url |
https://repositorio.unal.edu.co/handle/unal/41878 http://bdigital.unal.edu.co/31975/ |
dc.language.iso.spa.fl_str_mv |
spa |
language |
spa |
dc.relation.spa.fl_str_mv |
http://revistas.unal.edu.co/index.php/geocol/article/view/31302 |
dc.relation.ispartof.spa.fl_str_mv |
Universidad Nacional de Colombia Revistas electrónicas UN Geología Colombiana Geología Colombiana |
dc.relation.ispartofseries.none.fl_str_mv |
Geología Colombiana - An International Journal on Geosciences; Vol. 18 (1993); 65-73 Geología Colombiana; Vol. 18 (1993); 65-73 2357-3767 0072-0992 |
dc.relation.references.spa.fl_str_mv |
Ujueta L., Guillermo (1993) Lineamientos muzo, tunja y paipa en los departamentos de boyacá y casanare, colombia. Geología Colombiana - An International Journal on Geosciences; Vol. 18 (1993); 65-73 Geología Colombiana; Vol. 18 (1993); 65-73 2357-3767 0072-0992 . |
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 |
Departamento de Geociencias |
institution |
Universidad Nacional de Colombia |
bitstream.url.fl_str_mv |
https://repositorio.unal.edu.co/bitstream/unal/41878/1/31302-113377-1-PB.pdf https://repositorio.unal.edu.co/bitstream/unal/41878/2/31302-113377-1-PB.pdf.jpg |
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Repositorio Institucional Universidad Nacional de Colombia |
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