Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/245254
Share/Export:
logo share SHARE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
DC FieldValueLanguage
dc.contributor.authorNuñez-Cornu, Franciscoes_ES
dc.contributor.authorCórdoba, Diegoes_ES
dc.contributor.authorBandy, Williames_ES
dc.contributor.authorDañobeitia, Juan Josées_ES
dc.contributor.authorMortera-Gutierrez, Carloses_ES
dc.contributor.authorAlarcon, Edgares_ES
dc.contributor.authorNuñez, Dianaes_ES
dc.contributor.authorQuinteros Cartaya, Claudia Beatriz M.es_ES
dc.contributor.authorSuarez-Plascencia, Carloses_ES
dc.date.accessioned2021-07-05T11:07:13Z-
dc.date.available2021-07-05T11:07:13Z-
dc.date.issued2020-12-15-
dc.identifier.citationAmerican Geophysical Union Fall Meeting (2020)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/245254-
dc.descriptionAmerican Geophysical Union (AGU) Fall Meeting, 13-17 December 2021, New Orleanses_ES
dc.description.abstractThe geodynamic complexity in the interaction between Rivera, Cocos, and North American plates, is mainly evidenced by a high seismicity rate that unfavorably is not well located. In the framework of the TsuJal Project, a study of the passive seismic activity was carried out in this region, using data with a temporal seismic network with 25 Obsidian stations, deployed along the states of Nayarit, Jalisco and Colima, including the Islas Marías, in addition to the Jalisco Seismic Network (RESAJ), and 10 OBS type LCHEAPO 2000 with four channels, deployed and recovered by the BO El Puma in an array from the Islas Marías to off coast of the border of Colima and Michoacan states, in the period from 19th April to 7th November 2016. These networks allowed registering more than 2000 oceanic and continental earthquakes in the region, and will permit us to improve the quality of locations and design procedures for routine RESAJ offshore seismicity location. During the observation period, a seismic sequence occurred in the area between the Mesoamerican Trench and the Paleo-Rivera Transform Fault from May 7 to July 13 that included 22 earthquakes with a magnitude greater than 4.0, and one of magnitude 6.3 on June 7. The relocation of this seismic sequence offers a new vision on local tectonicses_ES
dc.language.isoenges_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.rightsclosedAccesses_ES
dc.titleThe TsuJal Amphibious Seismic Network: a Passive-Source seismic Experiment in Western Mexicoes_ES
dc.typecomunicación de congresoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.type.coarhttp://purl.org/coar/resource_type/c_5794es_ES
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.languageiso639-1en-
item.openairetypecomunicación de congreso-
Appears in Collections:(ICM) Comunicaciones congresos
(ICMAT) Comunicaciones congresos
(UTM) Comunicaciones congresos
Show simple item record

Page view(s)

50
checked on May 21, 2022

Google ScholarTM

Check


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.