3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion

The Southern terminus of the Rio Grande Rift region has been poorly defined in the geologic record, with few seismic studies that provide information on the deeper Rift structure. In consequence, important questions related to tectonic and lithospheric activity of the Rio Grande Rift remain unresolv...

Full description

Autores:
Sosa Aguirre, Uram Anibal
Thompson, Lennox
Herrmann, Robert B.
Romero, Rodrigo
Velasco, Aaron A.
Tipo de recurso:
Article of investigation
Fecha de publicación:
2014
Institución:
Universidad ICESI
Repositorio:
Repositorio ICESI
Idioma:
spa
OAI Identifier:
oai:repository.icesi.edu.co:10906/78327
Acceso en línea:
http://www.scopus.com/inward/record.url?eid=2-s2.0-84926278815&partnerID=tZOtx3y1
http://hdl.handle.net/10906/78327
https://doi.org/10.1016/j.epsl.2014.06.002
Palabra clave:
Rio Grande Rift
Computational geosciences
Jemez lineament
Automatización y sistemas de control
Automation
Control system
Rights
openAccess
License
https://creativecommons.org/licenses/by-nc-nd/4.0/
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oai_identifier_str oai:repository.icesi.edu.co:10906/78327
network_acronym_str ICESI2
network_name_str Repositorio ICESI
repository_id_str
spelling Sosa Aguirre, Uram AnibalThompson, LennoxHerrmann, Robert B.Romero, RodrigoVelasco, Aaron A.uasosa@icesi.edu.coLat: 25 07 00 N grados minutos Lat: 25.1167 grados decimales Largo: 100 28 00 W grados minutos Largos: -100.4667 grados decimales2015-09-30T22:24:05Z2015-09-30T22:24:05Z2014-01-010012-821Xhttp://www.scopus.com/inward/record.url?eid=2-s2.0-84926278815&partnerID=tZOtx3y1http://hdl.handle.net/10906/78327https://doi.org/10.1016/j.epsl.2014.06.002instname: Universidad Icesireponame: Biblioteca Digitalrepourl: https://repository.icesi.edu.co/The Southern terminus of the Rio Grande Rift region has been poorly defined in the geologic record, with few seismic studies that provide information on the deeper Rift structure. In consequence, important questions related to tectonic and lithospheric activity of the Rio Grande Rift remain unresolved. To address some of these geological questions, we collect and analyze seismic data from 147 EarthScope Transportable Array (USArray) and other seismic stations in the region, to develop a 3-D crust and upper mantle velocity model. We apply a constrained optimization approach for joint inversion of surface wave and receiver functions using seismic S wave velocities as a model parameter. In particular, we compute receiver functions stacks based on ray parameter, and invert them jointly with collected surface wave group velocity dispersion observations. The inversions estimate 1-D seismic S-wave velocity profiles to 300 km depth, which are then interpolated to a 3-D velocity model using a Bayesian kriging scheme. Our 3-D models show a thin lower velocity crust anomaly along the southeastern Rio Grande Rift, a persistent low velocity anomaly underneath the Colorado Plateau and Basin and Range province, and another one at depth beneath the Jemez lineament, and the southern RGR.10 páginasDigitalspaElsevierFacultad de IngenieríaDepartamento de Matemáticas y EstadísticaEarth and Planetary Science Letters, Vol. 402, No. 15 -2014EL AUTOR, expresa que la obra objeto de la presente autorización es original y la elaboró sin quebrantar ni suplantar los derechos de autor de terceros, y de tal forma, la obra es de su exclusiva autoría y tiene la titularidad sobre éste. PARÁGRAFO: en caso de queja o acción por parte de un tercero referente a los derechos de autor sobre el artículo, folleto o libro en cuestión, EL AUTOR, asumirá la responsabilidad total, y saldrá en defensa de los derechos aquí autorizados; para todos los efectos, la Universidad Icesi actúa como un tercero de buena fe. Esta autorización, permite a la Universidad Icesi, de forma indefinida, para que en los términos establecidos en la Ley 23 de 1982, la Ley 44 de 1993, leyes y jurisprudencia vigente al respecto, haga publicación de este con fines educativos. Toda persona que consulte ya sea la biblioteca o en medio electrónico podrá copiar apartes del texto citando siempre la fuentes, es decir el título del trabajo y el autor.https://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessAtribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)http://purl.org/coar/access_right/c_abf2Rio Grande RiftComputational geosciencesJemez lineamentAutomatización y sistemas de controlAutomationControl system3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersioninfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_2df8fbb1Artículoinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/version/c_970fb48d4fbd8a85Comunidad Universidad Icesi - Investigadores40215127ORIGINALdocumento.htmldocumento.htmltext/html299http://repository.icesi.edu.co/biblioteca_digital/bitstream/10906/78327/1/documento.html0b3ace8967d8368916af850722911abcMD5110906/78327oai:repository.icesi.edu.co:10906/783272018-10-10 18:07:32.535Biblioteca Digital - Universidad icesicdcriollo@icesi.edu.co
dc.title.spa.fl_str_mv 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
title 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
spellingShingle 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
Rio Grande Rift
Computational geosciences
Jemez lineament
Automatización y sistemas de control
Automation
Control system
title_short 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
title_full 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
title_fullStr 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
title_full_unstemmed 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
title_sort 3-D structure of the Rio Grande Rift from 1-D constrained joint inversion of receiver functions and surface wave dispersion
dc.creator.fl_str_mv Sosa Aguirre, Uram Anibal
Thompson, Lennox
Herrmann, Robert B.
Romero, Rodrigo
Velasco, Aaron A.
dc.contributor.author.spa.fl_str_mv Sosa Aguirre, Uram Anibal
Thompson, Lennox
Herrmann, Robert B.
Romero, Rodrigo
Velasco, Aaron A.
dc.subject.spa.fl_str_mv Rio Grande Rift
Computational geosciences
Jemez lineament
Automatización y sistemas de control
Automation
Control system
topic Rio Grande Rift
Computational geosciences
Jemez lineament
Automatización y sistemas de control
Automation
Control system
description The Southern terminus of the Rio Grande Rift region has been poorly defined in the geologic record, with few seismic studies that provide information on the deeper Rift structure. In consequence, important questions related to tectonic and lithospheric activity of the Rio Grande Rift remain unresolved. To address some of these geological questions, we collect and analyze seismic data from 147 EarthScope Transportable Array (USArray) and other seismic stations in the region, to develop a 3-D crust and upper mantle velocity model. We apply a constrained optimization approach for joint inversion of surface wave and receiver functions using seismic S wave velocities as a model parameter. In particular, we compute receiver functions stacks based on ray parameter, and invert them jointly with collected surface wave group velocity dispersion observations. The inversions estimate 1-D seismic S-wave velocity profiles to 300 km depth, which are then interpolated to a 3-D velocity model using a Bayesian kriging scheme. Our 3-D models show a thin lower velocity crust anomaly along the southeastern Rio Grande Rift, a persistent low velocity anomaly underneath the Colorado Plateau and Basin and Range province, and another one at depth beneath the Jemez lineament, and the southern RGR.
publishDate 2014
dc.date.issued.none.fl_str_mv 2014-01-01
dc.date.accessioned.none.fl_str_mv 2015-09-30T22:24:05Z
dc.date.available.none.fl_str_mv 2015-09-30T22:24:05Z
dc.type.none.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.doi.none.fl_str_mv https://doi.org/10.1016/j.epsl.2014.06.002
dc.identifier.instname.none.fl_str_mv instname: Universidad Icesi
dc.identifier.reponame.none.fl_str_mv reponame: Biblioteca Digital
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url http://www.scopus.com/inward/record.url?eid=2-s2.0-84926278815&partnerID=tZOtx3y1
http://hdl.handle.net/10906/78327
https://doi.org/10.1016/j.epsl.2014.06.002
dc.language.iso.none.fl_str_mv spa
language spa
dc.relation.ispartof.eng.fl_str_mv Earth and Planetary Science Letters, Vol. 402, No. 15 -2014
dc.rights.uri.none.fl_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.rights.accessrights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.license.none.fl_str_mv Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)
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Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)
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eu_rights_str_mv openAccess
dc.format.extent.none.fl_str_mv 10 páginas
dc.format.medium.none.fl_str_mv Digital
dc.coverage.spatial.none.fl_str_mv Lat: 25 07 00 N grados minutos Lat: 25.1167 grados decimales Largo: 100 28 00 W grados minutos Largos: -100.4667 grados decimales
dc.publisher.spa.fl_str_mv Elsevier
dc.publisher.faculty.spa.fl_str_mv Facultad de Ingeniería
dc.publisher.department.spa.fl_str_mv Departamento de Matemáticas y Estadística
institution Universidad ICESI
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