dor_id: 4132968

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/321/307

100.1.#.a: Garduño-monroy, V. H.; Pérez-lopez, R.; Israde-alcantara, I.; Rodríguez-pascua, M. A.; Szynkaruk, E.; Hernández-madrigal, V. M.; García-zepeda, M. L.; Corona-chávez, P.; Ostroumov, M.; Medina-vega, V. H.; García-estrada, G.; Carranza, O.; Lopez-granados, E.; Mora Chaparro, J. C.

524.#.#.a: Garduño-monroy, V. H., et al. (2009). Paleoseismology of the southwestern Morelia-Acambay fault system, central Mexico. Geofísica Internacional; Vol. 48 Núm. 3: Julio 1, 2009; 319-335. Recuperado de https://repositorio.unam.mx/contenidos/4132968

245.1.0.a: Paleoseismology of the southwestern Morelia-Acambay fault system, central Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2009

264.#.1.c: 2009-07-01

653.#.#.a: Sismicidad, Morelia; Tectónica activa; fallas normales; Cuitzeo; Seismicity; Morelia; Active Tectonic; normal fault; Cuitzeo

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/321

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/321

041.#.7.h: spa

520.3.#.a: Fr The Morelia–Acambay Fault System (MAFS) consists of a sequence of E–W and NNE–SSW trending normal faults within the Trans–Mexican Volcanic Belt. The fault system is associated to the Chapala, Zacapu, Cuitzeo, Maravatio and Acambay lacustrine depressions. The E–W faults of MAFS appear to be 7–9 million yr old while the NNW–SSE faults are older and were reactivated producing stepped east–west geometry with a transtensional–right hand deformation.Seismic magnitudes of the E–W structures in the Morelia–Cuitzeo region are estimated. Cartography, structural geology, and trench stratigraphy of these faults suggest Holocene activity. Historical earthquakes disrupted paleosols containing Pirinda–Purepecha shards. These Historical earthquakes are also imprinted in seisms along E–W faults at Los Azufres geothermal field. In the Pátzcuaro region, the E–W structures are also linked to strong seismic events occurred during prehistoric and historical times. The Jaracuaro lacustrine sequence in the southern Patzcuaro Lake contains evidence at least three important earthquakes (PostClassic, 1845 and 1858) and a possible tsunami associated to the 1858 event. The magnitude of this earthquake was estimated at ~7.3. An earthquake of this magnitude would damage a density populated area of Michoacán State. On October 17, 2007, three small earthquakes were felt in Morelia associated to normal E–W fault mechanisms of Central Camionera Fault corroborating the seismic potential of MAFS in the TMBV.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.3.29

773.1.#.t: Geofísica Internacional; Vol. 48 Núm. 3: Julio 1, 2009; 319-335

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: 319-335

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

doi: https://doi.org/10.22201/igeof.00167169p.2009.48.3.29

handle: 00bfafef87c0f213

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

856.#.0.q: application/pdf

file_creation_date: 2009-08-04 21:17:41.0

file_modification_date: 2022-05-30 15:02:19.0

file_creator: V. H. Garduño–Monroy

file_name: cc40cc16b156b03247a1e0095b62e48a30ef15c35538079e4901353b246de0c1.pdf

file_pages_number: 17

file_format_version: application/pdf; version=1.4

file_size: 1834900

245.1.0.b: Paleoseismology of the southwestern Morelia-Acambay fault system, central Mexico

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