dor_id: 4132980

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

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

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

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

336.#.#.b: 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

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

590.#.#.b: Concentrador

883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

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

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

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

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/377/380

100.1.#.a: Carciumaru, Dana; Ortega, Roberto

524.#.#.a: Carciumaru, Dana, et al. (2011). On the origin of low angle normal faulting in the southern rio grande rift. Geofísica Internacional; Vol. 50 Núm. 2: Abril 1, 2011; 177­-190. Recuperado de https://repositorio.unam.mx/contenidos/4132980

245.1.0.a: On the origin of low angle normal faulting in the southern rio grande rift

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2011

264.#.1.c: 2011-04-01

653.#.#.a: inversión de esfuerzos; falla normal de bajo ángulo; correccion angular por basculamiento; rift del Rio Grande; stress inversion; low angle normal faults; back tilting; Rio Grande rift

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/377

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/377

041.#.7.h: spa

520.3.#.a: We reconstruct the stress regime in the East Potrillo and Franklin Mountains. Using modern numerical techniques the stress field and the tectonic history of this region is discussed and extensional veins were compared with the general stress field. The majority of faults were reactivated during the first Rio Grande rift extensional event and occurrence of extensive tilting and rotations occurred. In the East Potrillo Mountains, back tilting by W25°SE and W45°SE oriented along strikes of N30°W are required in order to obtain two homogeneous stress fields. The corrected fault plane shows a significant oblique component in both stress fields. The first stress field corresponds to a fault reactivation with σl and σ3 oriented N78°E and N69°E respectively, whereas the second stress field is related to the youngest fault oriented N64°W and N61°E respectively. In the Franklin Mountains, tilting is less significant; however two stress fields with similar orientations but different phi values are recognized. The post –Laramide stress history of the region is controlled by different extensional events that influenced the preexisting structures and generated other young fault systems.doi: https://doi.org/10.22201/igeof.00167169p.2011.50.2.137

773.1.#.t: Geofísica Internacional; Vol. 50 Núm. 2: Abril 1, 2011; 177­-190

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

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 177­-190

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

doi: https://doi.org/10.22201/igeof.00167169p.2011.50.2.137

handle: 28fd4da9b3c71f20

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-04 19:13:41.0

file_modification_date: 2022-07-04 19:13:41.0

file_creator: Carciumaru D.

file_name: d64b1b8951eefae319379ef1964fd676c355ae7c49774d99936c7cc4413116df.pdf

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file_size: 1309151

245.1.0.b: On the origin of low angle normal faulting in the southern rio grande rift

last_modified: 2023-06-20 16:00:00

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

On the origin of low angle normal faulting in the southern rio grande rift

Carciumaru, Dana; Ortega, Roberto

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

Carciumaru, Dana, et al. (2011). On the origin of low angle normal faulting in the southern rio grande rift. Geofísica Internacional; Vol. 50 Núm. 2: Abril 1, 2011; 177­-190. Recuperado de https://repositorio.unam.mx/contenidos/4132980

Descripción del recurso

Autor(es)
Carciumaru, Dana; Ortega, Roberto
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
On the origin of low angle normal faulting in the southern rio grande rift
Fecha
2011-04-01
Resumen
We reconstruct the stress regime in the East Potrillo and Franklin Mountains. Using modern numerical techniques the stress field and the tectonic history of this region is discussed and extensional veins were compared with the general stress field. The majority of faults were reactivated during the first Rio Grande rift extensional event and occurrence of extensive tilting and rotations occurred. In the East Potrillo Mountains, back tilting by W25°SE and W45°SE oriented along strikes of N30°W are required in order to obtain two homogeneous stress fields. The corrected fault plane shows a significant oblique component in both stress fields. The first stress field corresponds to a fault reactivation with σl and σ3 oriented N78°E and N69°E respectively, whereas the second stress field is related to the youngest fault oriented N64°W and N61°E respectively. In the Franklin Mountains, tilting is less significant; however two stress fields with similar orientations but different phi values are recognized. The post –Laramide stress history of the region is controlled by different extensional events that influenced the preexisting structures and generated other young fault systems.doi: https://doi.org/10.22201/igeof.00167169p.2011.50.2.137
Tema
inversión de esfuerzos; falla normal de bajo ángulo; correccion angular por basculamiento; rift del Rio Grande; stress inversion; low angle normal faults; back tilting; Rio Grande rift
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces