Estimación de las discontinuidades de la Zona de Transición del Manto en el noroccidente de Suramérica a partir del análisis de la Función Receptora de onda P

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dc.contributor.advisorVargas Jimenez, Carlos Alberto
dc.contributor.authorCubillos Gordillo, Jorge Enrique
dc.date.accessioned2024-12-09T20:45:44Z
dc.date.available2024-12-09T20:45:44Z
dc.date.issued2022-02
dc.descriptionilustraciones, graficas, mapas, tablasspa
dc.description.abstractLa zona de transición del manto está limitada por dos discontinuidades sísmicas a 410 y 660 kilómetros, _estas son visualizadas en la parte noroccidental de Suramérica mediante el uso de la técnica de función receptora e información sismológica, la cual ha sido registrada durante mas de 20 años por la red sismológica nacional de Colombia. Se observaron variaciones importantes y espacialmente sistemática en las profundidades de las discontinuidades. La profundidad promedio para los límites de la zona de transición del manto son 412±5.3 y 671±5.9 con un espesor promedio es de 258±6.5 km, el cual es cercano al valor promedio global. El bajo coeficiente de correlación de las profundidades indica que la variación de estas profundidades es significativa. El aumento en el espesor de la zona de transición del manto en algunas zonas es causado por la subducción de la placa Nazca y la placa Caribe bajo la placa Suramérica. Por otro lado, el adelgazamiento de la zona de transición del manto bajo la placa Nazca posiblemente se debe a la presencia del ridge de Malpelo. Estas observaciones combinadas con los resultados de investigaciones de tomografías sísmicas pudieron confirmar la interacción entre las placas Nazca y Caribe con el manto superior y la hidratación de la zona de transición del manto.spa
dc.description.abstractMantle transition zone is delimited by two seismic discontinuities at 410 and 660 kilometers, these are imaged beneath the northwestern corner of South America using the receiver function technique and a seismological record of 20 years compiled by the red sismol´ogica nacional de Colombia. Significant and spatially systematic depth variations in the discontinuities were observed. The mean depth for the mantle transition limits are 412±5.3 and 671±5.9, and mean thickness of 258±6.5, this value doesn’t differ from the global average. The low correlation between the discontinuities is caused by the significant depth variation. The thicker mantle transition zone in some areas is because the Nazca and Caribe plates subduction under South America plate. On the other hand, mantle transition zone thinning beneath the Nazca plate possible is due to the Malpelo ridge presence. These observations together with seismic tomography investigations could confirm the interaction of Nazca and Caribe plate within the upper mantle and mantle transition zone hydration.eng
dc.description.degreelevelMaestríaspa
dc.description.degreenameMagíster en Ciencias - Geofísicaspa
dc.description.researchareaSismotectónicaspa
dc.format.extentx, 159 páginasspa
dc.format.mimetypeapplication/pdfspa
dc.identifier.instnameUniversidad Nacional de Colombiaspa
dc.identifier.reponameRepositorio Institucional Universidad Nacional de Colombiaspa
dc.identifier.repourlhttps://repositorio.unal.edu.co/spa
dc.identifier.urihttps://repositorio.unal.edu.co/handle/unal/87282
dc.language.isospaspa
dc.publisherUniversidad Nacional de Colombiaspa
dc.publisher.branchUniversidad Nacional de Colombia - Sede Bogotáspa
dc.publisher.facultyFacultad de Cienciasspa
dc.publisher.placeBogotá, Colombiaspa
dc.publisher.programBogotá - Ciencias - Maestría en Ciencias - Geofísicaspa
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dc.rights.accessrightsinfo:eu-repo/semantics/openAccessspa
dc.rights.licenseReconocimiento 4.0 Internacionalspa
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/spa
dc.subject.lembDIBUJO TOPOGRAFICO
dc.subject.lembTopographical drawing
dc.subject.lembMEDICION DE SUPERFICIES
dc.subject.lembArea measurement
dc.subject.proposalFunción receptoraspa
dc.subject.proposalzona de transición del mantospa
dc.subject.proposalsubducciónspa
dc.subject.proposaltelesísmospa
dc.subject.proposaldiscontinuidad sísmicaspa
dc.subject.proposalSuraméricaspa
dc.subject.proposalReceiver functioneng
dc.subject.proposalTeleseismeng
dc.subject.proposalSeismic discontinuityeng
dc.subject.proposalMantle transition zoneeng
dc.subject.proposalSubductioneng
dc.subject.proposalSouth Americaeng
dc.titleEstimación de las discontinuidades de la Zona de Transición del Manto en el noroccidente de Suramérica a partir del análisis de la Función Receptora de onda Pspa
dc.title.translatedEstimation of Mantle Transition Zone discontinuities in northwestern Southamerica from P wave receiver function analysiseng
dc.typeTrabajo de grado - Maestríaspa
dc.type.coarhttp://purl.org/coar/resource_type/c_bdccspa
dc.type.coarversionhttp://purl.org/coar/version/c_ab4af688f83e57aaspa
dc.type.contentTextspa
dc.type.driverinfo:eu-repo/semantics/masterThesisspa
dc.type.redcolhttp://purl.org/redcol/resource_type/TMspa
dc.type.versioninfo:eu-repo/semantics/acceptedVersionspa
dcterms.audience.professionaldevelopmentInvestigadoresspa
oaire.accessrightshttp://purl.org/coar/access_right/c_abf2spa

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