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510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

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

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336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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

351.#.#.b: Geofísica Internacional

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

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

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/528/545

100.1.#.a: Quintanilla M., Ana Luz; Suarez V., Francisco

524.#.#.a: Quintanilla M., Ana Luz, et al. (1994). Fuente de calor en el campo geotérmico de Cerro Prieto y su relación con la anomalía magnética Nuevo León, México. Geofísica Internacional; Vol. 33 Núm. 4: Octubre 1, 1994; 575-584. Recuperado de https://repositorio.unam.mx/contenidos/4132503

245.1.0.a: Fuente de calor en el campo geotérmico de Cerro Prieto y su relación con la anomalía magnética Nuevo León, México

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1994

264.#.1.c: 1994-10-01

653.#.#.a: Centro de dispersión; anomalía magnética; Cerro Prieto; geotermia; fuente de calor; Spreading center; magnetic anomaly; Cerro Prieto; heat source; geothermics

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-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/528

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041.#.7.h: spa

520.3.#.a: The Cerro Prieto geothermal system located within the Salton Trough province is one of the northernmost of a serie of active hydrothermal systems found along the East Pacific Rise-San Andreas Fault zone plate boundary transition. Several models have been developed in an attempt to understand the tectonic process which creates the geothermal environment in the area. Among such models is the one of Goldstein et al., (1984) which used the magnetic data and some petrographic analysis available. They proposed that the so called Nuevo León magnetic anomaly is produced by a prismatic body located at 3.8 km of depth which is constituted by gabbros and peridotites. Using the magnetic data and combining with the new petrological results from rock samples collected in recent boreholes from the field, and based upon the calculated thermal gradient, we have modified the Goldstein et al. (1984) model. The Nuevo Leon magnetic anomaly is produced not by one body but by two located at different depths and with different dimensions. In the shallower one, the top is located at 4.5 km and its base at 7 km deep, this is slightly tilted to the north. In the second body, the upper part is at 5 km deep and the base at 8 km. Both of them are gabbros in composition. Considering the results obtained and based upon the thermal gradient, the mixing zone is located at 11 km depth and the mafic plutonic bodies are considered part of the thermal source in the area.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.4.593

773.1.#.t: Geofísica Internacional; Vol. 33 Núm. 4: Octubre 1, 1994; 575-584

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

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doi: https://doi.org/10.22201/igeof.00167169p.1994.33.4.593

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harvesting_date: 2023-06-20 16:00:00.0

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file_modification_date: 2022-07-07 17:30:37.0

file_creator: Ana Luz Quintanilla

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245.1.0.b: Fuente de calor en el campo geotérmico de Cerro Prieto y su relación con la anomalía magnética Nuevo León, México

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Artículo

Fuente de calor en el campo geotérmico de Cerro Prieto y su relación con la anomalía magnética Nuevo León, México

Quintanilla M., Ana Luz; Suarez V., Francisco

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

Quintanilla M., Ana Luz, et al. (1994). Fuente de calor en el campo geotérmico de Cerro Prieto y su relación con la anomalía magnética Nuevo León, México. Geofísica Internacional; Vol. 33 Núm. 4: Octubre 1, 1994; 575-584. Recuperado de https://repositorio.unam.mx/contenidos/4132503

Descripción del recurso

Autor(es)
Quintanilla M., Ana Luz; Suarez V., Francisco
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Fuente de calor en el campo geotérmico de Cerro Prieto y su relación con la anomalía magnética Nuevo León, México
Fecha
1994-10-01
Resumen
The Cerro Prieto geothermal system located within the Salton Trough province is one of the northernmost of a serie of active hydrothermal systems found along the East Pacific Rise-San Andreas Fault zone plate boundary transition. Several models have been developed in an attempt to understand the tectonic process which creates the geothermal environment in the area. Among such models is the one of Goldstein et al., (1984) which used the magnetic data and some petrographic analysis available. They proposed that the so called Nuevo León magnetic anomaly is produced by a prismatic body located at 3.8 km of depth which is constituted by gabbros and peridotites. Using the magnetic data and combining with the new petrological results from rock samples collected in recent boreholes from the field, and based upon the calculated thermal gradient, we have modified the Goldstein et al. (1984) model. The Nuevo Leon magnetic anomaly is produced not by one body but by two located at different depths and with different dimensions. In the shallower one, the top is located at 4.5 km and its base at 7 km deep, this is slightly tilted to the north. In the second body, the upper part is at 5 km deep and the base at 8 km. Both of them are gabbros in composition. Considering the results obtained and based upon the thermal gradient, the mixing zone is located at 11 km depth and the mafic plutonic bodies are considered part of the thermal source in the area.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.4.593
Tema
Centro de dispersión; anomalía magnética; Cerro Prieto; geotermia; fuente de calor; Spreading center; magnetic anomaly; Cerro Prieto; heat source; geothermics
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces