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...

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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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repository_id_str
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_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
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dc.type.content.spa.fl_str_mv Text
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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
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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
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