Near-realtime source analysis of the
Mendoza, Carlos
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
dor_id: 4132208
506.#.#.a: Público
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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
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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/517/535
100.1.#.a: Mendoza, Carlos
524.#.#.a: Mendoza, Carlos (2014). Near-realtime source analysis of the. Geofísica Internacional; Vol. 53 Núm. 2: Abril 1, 2014; 211-220. Recuperado de https://repositorio.unam.mx/contenidos/4132208
245.1.0.a: Near-realtime source analysis of the
502.#.#.c: Universidad Nacional Autónoma de México
561.1.#.a: Instituto de Geofísica, UNAM
264.#.0.c: 2014
264.#.1.c: 2014-04-01
653.#.#.a: propiedades de la fuente del terremoto; inversión de fallas finitas; ondas P telesísmicas; earthquake source properties; finite-fault inversion; teleseismic P waves
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/517
001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/517
041.#.7.h: spa
520.3.#.a: We apply a single-step, finite-fault analysis procedure to derive a coseismic slip model for the large MW 7.4 Ometepec-Pinotepa Nacional, Mexico earthquake of 20 March 2012, using teleseismic P waveforms recorded by the Global Seismographic Network. The inversion is conducted in near-realtime using source parameters available from the USGS/NEIC and the Global Centroid Moment Tensor (gCMT) project. The fault orientation and slip angle are obtained from the gCMT mechanism assuming that the fault coincides with the shallow-dipping nodal plane. The fault dimensions and maximum rise time are based on the magnitude reported for the event. Teleseismic data from the USGS/ NEIC Continuous Waveform Buffer database are used in the inversion with record start times set to the P-wave arrivals used to compute the earthquake hypocenter. The inversion is stabilized by requiring a smooth transition of slip across the fault while minimizing the seismic moment. These constraints are applied using a smoothing weight that is estimated from the inverse problem, allowing the recovery of the least-complicated rupture history in a single step. Inversion of the deconvolved, ground-displacement waveforms reveals a simple, circular rupture similar in extent to the source identified by the USGS/NEIC using bodyand surface-wave data, indicating that the teleseismic P waves can provide a first-order source model for the event in near-realtime. Additional inversions conducted using velocity records identify a more-detailed rupture model characterized by an elliptical 2500 km2 source region extending updip and downdip from the hypocenter. This elliptical source preserves the orientation and overall dimensions of a dual-source slip model obtained recently by other investigators using local strong motions and global seismic waveforms. The results indicate that velocity waveforms could provide additional details of the earthquake rupture in near-realtime, finite-fault inversions using teleseismic P waves.doi: https://doi.org/10.1016/S0016-7169(14)71501-6
773.1.#.t: Geofísica Internacional; Vol. 53 Núm. 2: Abril 1, 2014; 211-220
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: 211-220
264.#.1.b: Instituto de Geofísica, UNAM
doi: https://doi.org/10.1016/S0016-7169(14)71501-6
handle: 6558a9ca13cc7e1c
harvesting_date: 2023-06-20 16:00:00.0
856.#.0.q: application/pdf
file_creation_date: 2014-04-07 17:39:13.0
file_modification_date: 2022-07-08 16:00:09.0
file_creator: Carlos Mendoza
file_name: 68057e77a0ba9e48116339264fe77d5ac0e2492f648e03541a3d6a898a4dc9c6.pdf
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245.1.0.b: Near-realtime source analysis of the 20 March 2012 Ometepec- Pinotepa Nacional, Mexico earthquake
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
Mendoza, Carlos
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
Mendoza, Carlos (2014). Near-realtime source analysis of the. Geofísica Internacional; Vol. 53 Núm. 2: Abril 1, 2014; 211-220. Recuperado de https://repositorio.unam.mx/contenidos/4132208