dor_id: 4133398

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/1239/1219

100.1.#.a: Castro, Raúl R.; Clayton, Robert; Hauksson, Egill; Stock, Joann

524.#.#.a: Castro, Raúl R., et al. (2017). Observations of remotely triggered seismicity in Salton Sea and Coso geothermal regions, Southern California, USA, after big (MW>7.8) teleseismic earthquakes. Geofísica Internacional; Vol. 56 Núm. 3: Julio 1, 2017; 269-286. Recuperado de https://repositorio.unam.mx/contenidos/4133398

245.1.0.a: Observations of remotely triggered seismicity in Salton Sea and Coso geothermal regions, Southern California, USA, after big (MW>7.8) teleseismic earthquakes

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2017

264.#.1.c: 2017-07-01

653.#.#.a: disparo remoto; sismicidad del sur de California; USA; campo geotérmico Coso; campo geotérmico Salton Sea; remote triggering; seismicity southern California; USA; Coso geothermal field; Salton Sea geothermal field

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/1239

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1239

041.#.7.h: spa

520.3.#.a: A relocated catalog was used to search for changes in seismicity rate in the Salton Sea and the Coso geothermal regions, southern California, USA, during and after large (MW>7.8) teleseismic earthquakes. Seismicity in these two regions was analyzed within 30-day windows before and after the occurrence of five major earthquakes: the 2002 Denali fault, Alaska (MW7.9); the 2004 Sumatra-Andama (MW9.2); the 2010 Central Chile (MW8.8); the 2011 Tohoku-Oki, Japan (MW9.1); and the 2012 Offshore Northern Sumatra (Mw8.6) earthquakes. The Denali (MW7.9) earthquake coincided with an increase in seismicity in the Salton Sea region the day when this remote event occurred, indicating that instantaneous triggered seismicity was likely related with the passage of its surface waves. However, in the Coso region the seismicity rate remained approximately constant during the 30-day observation period. The seismicity after the 2004 Sumatra-Andaman (MW9.2) earthquake increased in both regions 9 days after the megaearthquake. The seismicity after the 2010 Chile (MW8.8) earthquake increased in both regions approximately 14 days after the remote event. The seismicity in Salton Sea and Coso regions increased 17 and 14 days, respectively, after the 2011 Japan (MW9.1) earthquake, suggesting that delayed triggered seismicity was induced after the passage of the surface waves in both regions. Similarly, 6 and 16 days after the 2012 northern Sumatra (MW8.6) earthquake the seismicity also increased in Salton Sea and Coso regions, respectively. These observations can be interpreted as evidence of instantaneous and delayed dynamic triggering induced by large remote earthquakes. The maximum magnitude of the delayed triggered swarm increased with the strength (M0/D) of the mega-earthquake and, the stronger the remote earthquake, the longer the delay time.doi: https://doi.org/10.22201/igeof.00167169p.2017.56.3.1817

773.1.#.t: Geofísica Internacional; Vol. 56 Núm. 3: Julio 1, 2017; 269-286

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: 269-286

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

doi: https://doi.org/10.22201/igeof.00167169p.2017.56.3.1817

handle: 00ddbdad09fd2a21

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

856.#.0.q: application/pdf

file_creation_date: 2018-02-01 19:35:07.0

file_modification_date: 2022-04-08 15:23:58.0

file_creator: Raúl R. Castro

file_name: 67319b2509adca24741487d0b3caa78d183163c574831bce488867873f87b018.pdf

file_pages_number: 18

file_format_version: application/pdf; version=1.4

file_size: 1072801

245.1.0.b: Observations of remotely triggered seismicity in Salton Sea and Coso geothermal regions, Southern California, USA, after big (MW>7.8) teleseismic earthquakes

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

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

license_type: by-nc-sa

No entro en nada

No entro en nada 2