Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR)
The Sierra Nevada de Santa Marta (SNSM) is characterized for being the highest mountainous coastal system on the planet (Montes et al., 2005). It is a massif located in northeastern Colombia, between the departments of Magdalena, La Guajira, and Cesar. Its structure, triangular in shape, is distingu...
- Autores:
-
Moreno Soler, María Alejandra
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2017
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/61562
- Acceso en línea:
- http://hdl.handle.net/1992/61562
- Palabra clave:
- Interferometría
Radar de apertura sintética
Superficies
Tecnología de satélites en recursos de la tierra
- Rights
- openAccess
- License
- http://creativecommons.org/licenses/by-nc-sa/4.0/
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dc.title.spa.fl_str_mv |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
title |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
spellingShingle |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) Interferometría Radar de apertura sintética Superficies Tecnología de satélites en recursos de la tierra |
title_short |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
title_full |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
title_fullStr |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
title_full_unstemmed |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
title_sort |
Modelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR) |
dc.creator.fl_str_mv |
Moreno Soler, María Alejandra |
dc.contributor.advisor.none.fl_str_mv |
Pearse, Jillian |
dc.contributor.author.none.fl_str_mv |
Moreno Soler, María Alejandra |
dc.subject.keyword.spa.fl_str_mv |
Interferometría Radar de apertura sintética Superficies Tecnología de satélites en recursos de la tierra |
topic |
Interferometría Radar de apertura sintética Superficies Tecnología de satélites en recursos de la tierra |
description |
The Sierra Nevada de Santa Marta (SNSM) is characterized for being the highest mountainous coastal system on the planet (Montes et al., 2005). It is a massif located in northeastern Colombia, between the departments of Magdalena, La Guajira, and Cesar. Its structure, triangular in shape, is distinguished for being an independent mountainous body of the main mountain ranges of the Colombian territory (Tschanz et al., 1974). In Central America and South America, the international project CASA GPS was established in 1988 with the sponsorship of NSF, NASA and the National Science Foundation of the United States. During that same year, the Colombian Geological Service with the University of South Carolina established a campaign for the northern part of the country (from the 6À of latitude). In the area, five stations were located in: Rionegro, Montería, Cartagena, Valledupar, and Bucaramanga with results of displacement towards the northeast, which is related to the influence of the collision between Panama and Costa Rica (Mora et al., 2002). This GPS network technique is the most accurate, however, in order to be able to study the SNSM more quickly and efficiently, it is necessary to use a method that covers a larger area to help solve the multiple sources of deformation that are present (Pritchard, 2004). Considering the information described above, it is necessary to carry out an analysis of the geological evolution of this area by processing multiple satellite images. In this project, the deformation of the SNSM is described during 2016 taking into account Húctor Mora's approach, which establishes that the northern part of the country is moving towards the northeast. For this, the images will be processed with Isce, a program based on InSAR which allows to describe superficial deformations as small as one centimeter by comparing the phase of two images obtained at different times.--Tomado del Formato de Documento de Grado. |
publishDate |
2017 |
dc.date.issued.spa.fl_str_mv |
2017 |
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2022-09-26T22:26:09Z |
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2022-09-26T22:26:09Z |
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Trabajo de grado - Pregrado |
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http://purl.org/coar/resource_type/c_7a1f |
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Universidad de los Andes |
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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_abf2Pearse, Jillianvirtual::5636-1Moreno Soler, María Alejandra6c0c424e-06a8-457c-a166-58d244e69ae45002022-09-26T22:26:09Z2022-09-26T22:26:09Z2017http://hdl.handle.net/1992/61562instname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/795277-1001The Sierra Nevada de Santa Marta (SNSM) is characterized for being the highest mountainous coastal system on the planet (Montes et al., 2005). It is a massif located in northeastern Colombia, between the departments of Magdalena, La Guajira, and Cesar. Its structure, triangular in shape, is distinguished for being an independent mountainous body of the main mountain ranges of the Colombian territory (Tschanz et al., 1974). In Central America and South America, the international project CASA GPS was established in 1988 with the sponsorship of NSF, NASA and the National Science Foundation of the United States. During that same year, the Colombian Geological Service with the University of South Carolina established a campaign for the northern part of the country (from the 6À of latitude). In the area, five stations were located in: Rionegro, Montería, Cartagena, Valledupar, and Bucaramanga with results of displacement towards the northeast, which is related to the influence of the collision between Panama and Costa Rica (Mora et al., 2002). This GPS network technique is the most accurate, however, in order to be able to study the SNSM more quickly and efficiently, it is necessary to use a method that covers a larger area to help solve the multiple sources of deformation that are present (Pritchard, 2004). Considering the information described above, it is necessary to carry out an analysis of the geological evolution of this area by processing multiple satellite images. In this project, the deformation of the SNSM is described during 2016 taking into account Húctor Mora's approach, which establishes that the northern part of the country is moving towards the northeast. For this, the images will be processed with Isce, a program based on InSAR which allows to describe superficial deformations as small as one centimeter by comparing the phase of two images obtained at different times.--Tomado del Formato de Documento de Grado.La Sierra Nevada de Santa Marta (SNSM) se caracteriza por ser el sistema montañoso litoral más alto del planeta (Montes et al., 2005). Es un macizo que se encuentra ubicado en el noreste de Colombia, entre los departamentos del Magdalena, La Guajira, y el Cesar. Su estructura, de forma triangular, se distingue por ser un cuerpo montañoso independiente de las principales cadenas montañosas del territorio colombiano (Tschanz et al., 1974). En Centro América y en Sur América se estableció el proyecto internacional CASA GPS en 1988, con patrocinio de la NSF, la NASA, y la National Science Foundation de Estados Unidos. Durante ese mismo año, el Servicio Geológico Colombiano con la Universidad de Carolina del Sur establecieron una campaña para la parte norte del país (desde los 6À de latitud). En la zona se localizaron cinco estaciones en: Rionegro, Montería, Cartagena, Valledupar, y Bucaramanga con resultados de desplazamiento hacia el noreste, lo que se relaciona con la influencia de la colisión que se presenta entre Panamá y Costa Rica (Mora et al., 2002). Esta técnica de red de GPS es de las más precisas, sin embargo, para poder estudiar de una forma más rápida y eficaz la SNSM, es necesario contar con un método que abarque un área más grande para ayudar a resolver las múltiples fuentes de deformación que puedan presentarse (Pritchard, 2004). Considerando la información anterior, es necesario realizar un análisis de la evolución geológica de esta zona mediante el procesamiento de imágenes satelitales. En este proyecto se estudiará la deformación de la SNSM durante el 2016 teniendo en cuenta lo planteado por Héctor Mora, lo cual establece que la parte norte del país se encuentra en movimiento hacia el noreste. Para ello se procesarán las imágenes con Isce, un programa basado en InSAR el cual permite describir deformaciones superficiales tan pequeñas como de un centímetro comparando la fase de dos imágenes obtenidas en diferentes momentos.--Tomado del Formato de Documento de Grado.GeocientíficoPregradoprincipalmente a colorapplication/pdfspaUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de GeocienciasModelo de deformación de la Sierra Nevada de Santa Marta a través del radar Interferométrico de Apertura Sintética (InSAR)Trabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_7a1fTexthttp://purl.org/redcol/resource_type/TPInterferometríaRadar de apertura sintéticaSuperficiesTecnología de satélites en recursos de la tierra201224826Publicationhttps://scholar.google.es/citations?user=51m_M7sAAAAJvirtual::5636-1https://scienti.minciencias.gov.co/cvlac/visualizador/generarCurriculoCv.do?cod_rh=0001556274virtual::5636-15a9bff40-dc9a-46f5-ac1b-acd72f765934virtual::5636-15a9bff40-dc9a-46f5-ac1b-acd72f765934virtual::5636-1TEXT12832.pdf.txt12832.pdf.txtExtracted texttext/plain57423https://repositorio.uniandes.edu.co/bitstreams/8537ae75-c905-4fb3-b27b-fa266399cd7c/download2d37a1616874d101a3f12d7c112544b0MD52THUMBNAIL12832.pdf.jpg12832.pdf.jpgIM Thumbnailimage/jpeg5398https://repositorio.uniandes.edu.co/bitstreams/25a20cd0-167d-46ed-9583-42f23a26a32c/download50b4758b87c8b1ff6e6967ed4b30738aMD53ORIGINAL12832.pdfapplication/pdf12450716https://repositorio.uniandes.edu.co/bitstreams/f3159ee0-4c6b-49d1-84a6-c75b49511c83/downloadd12c96e73db7f07ffe137e99cddfacfcMD511992/61562oai:repositorio.uniandes.edu.co:1992/615622024-03-13 12:59:22.21http://creativecommons.org/licenses/by-nc-sa/4.0/open.accesshttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.co |