dor_id: 4133508

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/375/378

100.1.#.a: Garduño-­monroy, Victor Hugo; Soria-­caballero, Diana Cinthia; Israde­-alcántara, Isabel; Hernández-madrigal, Víctor Manuel; Rodríguez-ramírez, Alejandro; Ostroumov, Mikhail; Rodríguez-pascua, Miguel Ángel; Chacon-torres, Arturo; Mora­-chaparro, Juan Carlos

524.#.#.a: Garduño-­monroy, Victor Hugo, et al. (2011). Evidence of tsunami events in the Paleolimnological record of Lake Pátzcuaro, Michoacán, Mexico. Geofísica Internacional; Vol. 50 Núm. 2: Abril 1, 2011; 147­-161. Recuperado de https://repositorio.unam.mx/contenidos/4133508

245.1.0.a: Evidence of tsunami events in the Paleolimnological record of Lake Pátzcuaro, Michoacán, Mexico

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: Tsunamis en lagos; sismicidad histórica; ostrácodos; lago de Pátzcuaro; Tsunamis lakes; historical seismicity; ostracodes; lake Pátzcuaro

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/375

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/375

041.#.7.h: spa

520.3.#.a: Modern Lake Pátzcuaro has a surface elevation of 2035 m a.s.l. Historically, it reached an elevation of 2041 m a.s.l., which isolated a portion of the island near the town of Jarácuaro in the southeastern part of the lake. Two trenches in the former island reveal similar tripartite stratigraphic sequences. In a 3.1 m deep trench, the sequence from bottom to top comprises Unit A constituted by folded and faulted diatom–rich clay and silt with beds of volcanic sand. These deposits are dated between 24 and 10 ky BP; Unit B constituted by a 10 of cm chaotic mixture of volcanic sand and lapilli with abundant remains of fish, bivalves, gastropods and ostracodes that is rests on above an erosional unconformity. The ostracodes include articulated valves with a mixture of deep–water pelagic species and attached littoral species. Highly fractured diatom shows a mixture of planktonic and benthic habitats. Fragments of ceramic artifacts dated to the Post–Classic Period (900 to 1520 AD) are abundant; Unit Cconstituted by a 20 cm thick unit of organic–rich argillaceous silt with remains of gastropods, seeds, angular lithoclasts and fragments of Post–Classic ceramic artifacts.Unit B suggests a catastrophic resedi mentation of lake floor deposits attributed to a tsunami. Unit C is consistent with sublacustrine conditions that are historically documented from 1858 to 1947. A tsunami in Lake Pátzcuaro in 1858 has been historically recorded. The tsunami was created either by fault movement or collapse of the SW flank of the island of Janitzio. The tsunami wave may have contributed to the rapid rise of Lake Pátzcuaro following the 1858 seismic event.doi: https://doi.org/10.22201/igeof.00167169p.2011.50.2.135

773.1.#.t: Geofísica Internacional; Vol. 50 Núm. 2: Abril 1, 2011; 147­-161

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: 147­-161

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

doi: https://doi.org/10.22201/igeof.00167169p.2011.50.2.135

handle: 492e09a2f3014fa8

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-04 19:10:42.0

file_modification_date: 2022-07-04 19:10:42.0

file_creator: Garduño-Monroy V.H.

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245.1.0.b: Evidence of tsunami events in the Paleolimnological record of Lake Pátzcuaro, Michoacán, 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

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