Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes
The sedimentary and volcano-sedimentary rocks of the Quebradagrande Complex on the northwestern margin of South America record the arc and its associated back-arc tectonic settings. Sixteen thin sections were analyzed revealing distinct lava facies from basic to intermediate compositions. Field rela...
- Autores:
-
Marín Jaramillo, Juan Pablo
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2018
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/39325
- Acceso en línea:
- http://hdl.handle.net/1992/39325
- Palabra clave:
- Tectónica de placas
Rocas sedimentarias
Estratigrafía
Rocas ígneas
Magmatismo
Quebradagrande (Colombia)
Geociencias
- Rights
- openAccess
- License
- http://creativecommons.org/licenses/by-nc-sa/4.0/
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Al consultar y hacer uso de este recurso, está aceptando las condiciones de uso establecidas por los autores.http://creativecommons.org/licenses/by-nc-sa/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Rojas-Agramonte, Yamirka14e92f52-bf9b-42e6-9733-47fdfefbd5a1400Cardona Molina, Agustíned72e406-b8d0-463b-a044-a6f094777dea500Marín Jaramillo, Juan Pabloc2e1ccb1-9eb0-43b0-95ab-b92ac1498a8d500Delgado Uribe, Adriana2020-06-10T16:10:34Z2020-06-10T16:10:34Z2018http://hdl.handle.net/1992/39325u821255.pdfinstname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/The sedimentary and volcano-sedimentary rocks of the Quebradagrande Complex on the northwestern margin of South America record the arc and its associated back-arc tectonic settings. Sixteen thin sections were analyzed revealing distinct lava facies from basic to intermediate compositions. Field relations, six stratigraphic sections and petrographic analysis allow the identification of three main lithofacies: Sedimentary, effusive and pyroclastic. Their spatial relation shows an east to west transition from deep ocean sediments, basic lava compositions and gravity flow pyroclastic deposits to shallower depositional environments, intermediate lava compositions and fall pyroclastic deposits. The results obtained in this study confirm the tectono-magmatic models previously proposed in which a para-autochthonous island arc along with a marginal basin were stablished for early to mid-Cretaceous ages"Las rocas sedimentarias y volcán-sedimentarias del Complejo de Quebradagrande en el margen noroeste de América del Sur registran el arco y sus configuraciones tectónicas de arco inverso asociadas. Se analizaron dieciséis secciones delgadas que revelan distintas facies de lava desde composiciones básicas a intermedias. Las relaciones de campo, seis secciones estratigráficas y el análisis petrográfico permiten la identificación de tres litofacies principales: sedimentarias, efusivas y piroclásticas. Su relación espacial muestra una transición de este a oeste de sedimentos oceánicos profundos, composiciones básicas de lava y depósitos piroclásticos de flujo por gravedad a entornos de deposición más bajos, composiciones de lava intermedia y depósitos piroclásticos de caída. Los resultados obtenidos en este estudio confirman los modelos tectono-magmáticos propuestos anteriormente en los cuales se establecieron un arco isleño para-autóctono junto con una cuenca marginal para las edades del Cretácico temprano al medio."--Tomado del Formato de Documento de GradoGeocientíficoPregrado28 hojasapplication/pdfengUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de Geocienciasinstname:Universidad de los Andesreponame:Repositorio Institucional SénecaDepositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern AndesTrabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesishttp://purl.org/coar/resource_type/c_7a1fhttp://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/TPTectónica de placasRocas sedimentariasEstratigrafíaRocas ígneasMagmatismoQuebradagrande (Colombia)GeocienciasPublicationTHUMBNAILu821255.pdf.jpgu821255.pdf.jpgIM Thumbnailimage/jpeg9564https://repositorio.uniandes.edu.co/bitstreams/111b422b-6c33-44e2-9732-0d6110402a87/download17e97b001fb4869af89661bca1f52561MD55ORIGINALu821255.pdfapplication/pdf4334745https://repositorio.uniandes.edu.co/bitstreams/b13286b6-941e-430d-bc06-411742371311/downloadfe9b05af63db6bb42ca967acbb5d3e7cMD51TEXTu821255.pdf.txtu821255.pdf.txtExtracted texttext/plain31804https://repositorio.uniandes.edu.co/bitstreams/755ef7bd-659c-40a6-9749-403ddd87e04a/download7613034b1d074347f46e79b9d577f8d1MD541992/39325oai:repositorio.uniandes.edu.co:1992/393252023-10-10 16:31:01.533http://creativecommons.org/licenses/by-nc-sa/4.0/open.accesshttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.co |
dc.title.es_CO.fl_str_mv |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
title |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
spellingShingle |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes Tectónica de placas Rocas sedimentarias Estratigrafía Rocas ígneas Magmatismo Quebradagrande (Colombia) Geociencias |
title_short |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
title_full |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
title_fullStr |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
title_full_unstemmed |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
title_sort |
Depositional environment of the Quebradagrande complex : implications for the early to mid-Cretaceous tectono-magmatic evolution of the northern Andes |
dc.creator.fl_str_mv |
Marín Jaramillo, Juan Pablo |
dc.contributor.advisor.none.fl_str_mv |
Rojas-Agramonte, Yamirka Cardona Molina, Agustín |
dc.contributor.author.none.fl_str_mv |
Marín Jaramillo, Juan Pablo |
dc.contributor.jury.none.fl_str_mv |
Delgado Uribe, Adriana |
dc.subject.keyword.es_CO.fl_str_mv |
Tectónica de placas Rocas sedimentarias Estratigrafía Rocas ígneas Magmatismo |
topic |
Tectónica de placas Rocas sedimentarias Estratigrafía Rocas ígneas Magmatismo Quebradagrande (Colombia) Geociencias |
dc.subject.armarc.none.fl_str_mv |
Quebradagrande (Colombia) |
dc.subject.themes.none.fl_str_mv |
Geociencias |
description |
The sedimentary and volcano-sedimentary rocks of the Quebradagrande Complex on the northwestern margin of South America record the arc and its associated back-arc tectonic settings. Sixteen thin sections were analyzed revealing distinct lava facies from basic to intermediate compositions. Field relations, six stratigraphic sections and petrographic analysis allow the identification of three main lithofacies: Sedimentary, effusive and pyroclastic. Their spatial relation shows an east to west transition from deep ocean sediments, basic lava compositions and gravity flow pyroclastic deposits to shallower depositional environments, intermediate lava compositions and fall pyroclastic deposits. The results obtained in this study confirm the tectono-magmatic models previously proposed in which a para-autochthonous island arc along with a marginal basin were stablished for early to mid-Cretaceous ages |
publishDate |
2018 |
dc.date.issued.none.fl_str_mv |
2018 |
dc.date.accessioned.none.fl_str_mv |
2020-06-10T16:10:34Z |
dc.date.available.none.fl_str_mv |
2020-06-10T16:10:34Z |
dc.type.spa.fl_str_mv |
Trabajo de grado - Pregrado |
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http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/bachelorThesis |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_7a1f |
dc.type.content.spa.fl_str_mv |
Text |
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http://purl.org/redcol/resource_type/TP |
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http://hdl.handle.net/1992/39325 |
dc.identifier.pdf.none.fl_str_mv |
u821255.pdf |
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reponame:Repositorio Institucional Séneca |
dc.identifier.repourl.spa.fl_str_mv |
repourl:https://repositorio.uniandes.edu.co/ |
url |
http://hdl.handle.net/1992/39325 |
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u821255.pdf instname:Universidad de los Andes reponame:Repositorio Institucional Séneca repourl:https://repositorio.uniandes.edu.co/ |
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eng |
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eng |
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http://creativecommons.org/licenses/by-nc-sa/4.0/ http://purl.org/coar/access_right/c_abf2 |
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openAccess |
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28 hojas |
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dc.publisher.es_CO.fl_str_mv |
Universidad de los Andes |
dc.publisher.program.es_CO.fl_str_mv |
Geociencias |
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Facultad de Ciencias |
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Departamento de Geociencias |
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