dor_id: 42008

506.#.#.a: Público

590.#.#.d: Cada artículo es evaluado mediante una revisión ciega única. Los revisores son externos nacionales e internacionales.

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT), Sistema Regional de Información en Línea para Revistas Científicas de América Latina, el Caribe, España y Portugal (Latindex), Scientific Electronic Library Online (SciELO), SCOPUS, Web Of Science (WoS)

561.#.#.u: http://www.geofisica.unam.mx/

650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: info:eu-repo/semantics/article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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883.#.#.a: Revistas UNAM

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883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial, UNAM

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/863/845

100.1.#.a: Madrid, J. A.; Traslosheros, C.

524.#.#.a: Madrid, J. A., et al. (1983). Un modelo sísmico preliminar lateralmente heterogéneo del campo geotérmico de Cerro Prieto Baja California Norte. Geofísica Internacional; Vol. 22 No. 4, 1983. Recuperado de https://repositorio.unam.mx/contenidos/42008

245.1.0.a: Un modelo sísmico preliminar lateralmente heterogéneo del campo geotérmico de Cerro Prieto Baja California Norte

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1983

264.#.1.c: 2012-09-22

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-ND 4.0 Internacional, https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode.es, fecha de asignación de la licencia 2012-09-22, para un uso diferente consultar al responsable jurídico del repositorio por medio de revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/863

001.#.#.#: oai:ojs.ojs.geofisica.unam.mx:article/863

041.#.7.h: spa

520.3.#.a: About 125 selected events recorded by the CICESE network at the Cerro Prieto area were used to study the underlying structure in terms of P-wave velocity. The events were chosen according to their position with respect to three nearly aligned stations and used to draw travel time curves for different parts of the profile. It is supposed that the structure under this profile is representative of the region of geothermal production. This analysis establishes a preliminary model of the structure, to be used for more detailed investigations and, at the same time, tests a simple ray tracing method for heterogeneous two-dimensional media. Since seismic events are natural phenomena, the results are highly dependent on the accuracy of previously determined locations. In some cases, the reported errors are great, in others the recordings are dubious or incomplete, so we considered the trend shown by hypocenters to cluster at specific depths. We hope to begin an event-relocation model-reparameterization cycle as soon as new data are available. Here we advance our conclusion that controlled source experiments with broader seismic arrays would help to clearly define boundaries. These in turn could be correlated to real geological structures, demonstrating the possible connection between transform fault systems such as San Jacinto-Elsinore, Imperial-Cerro Prieto. Similarly, faults associated with fluid conduction and other phenomena of geotectonic interest could be identified.

773.1.#.t: Geofísica Internacional; Vol. 22 No. 4 (1983)

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

046.#.#.j: 2020-10-20 00:00:00.000000

022.#.#.a: 0016-7169

310.#.#.a: Trimestral

264.#.1.b: Instituto de Geofísica, UNAM

758.#.#.1: http://revistagi.geofisica.unam.mx/index.php/RGI

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harvesting_date: 2020-09-23 00:00:00.0

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No entro en nada

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Artículo

Un modelo sísmico preliminar lateralmente heterogéneo del campo geotérmico de Cerro Prieto Baja California Norte

Madrid, J. A.; Traslosheros, C.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Madrid, J. A., et al. (1983). Un modelo sísmico preliminar lateralmente heterogéneo del campo geotérmico de Cerro Prieto Baja California Norte. Geofísica Internacional; Vol. 22 No. 4, 1983. Recuperado de https://repositorio.unam.mx/contenidos/42008

Descripción del recurso

Autor(es)
Madrid, J. A.; Traslosheros, C.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Un modelo sísmico preliminar lateralmente heterogéneo del campo geotérmico de Cerro Prieto Baja California Norte
Fecha
2012-09-22
Resumen
About 125 selected events recorded by the CICESE network at the Cerro Prieto area were used to study the underlying structure in terms of P-wave velocity. The events were chosen according to their position with respect to three nearly aligned stations and used to draw travel time curves for different parts of the profile. It is supposed that the structure under this profile is representative of the region of geothermal production. This analysis establishes a preliminary model of the structure, to be used for more detailed investigations and, at the same time, tests a simple ray tracing method for heterogeneous two-dimensional media. Since seismic events are natural phenomena, the results are highly dependent on the accuracy of previously determined locations. In some cases, the reported errors are great, in others the recordings are dubious or incomplete, so we considered the trend shown by hypocenters to cluster at specific depths. We hope to begin an event-relocation model-reparameterization cycle as soon as new data are available. Here we advance our conclusion that controlled source experiments with broader seismic arrays would help to clearly define boundaries. These in turn could be correlated to real geological structures, demonstrating the possible connection between transform fault systems such as San Jacinto-Elsinore, Imperial-Cerro Prieto. Similarly, faults associated with fluid conduction and other phenomena of geotectonic interest could be identified.
Idioma
spa
ISSN
0016-7169

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