Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century

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Trabajo presentado en el 8th International Symposium on Andean Geodynamics (ISAG), realizado en Quito-Ecuador, del 24-26 setiembre, 2019. Evento organizado por el Instituto Geofísico, Escuela Politécnica Nacional (IG-EPN) del Ecuador, y el French Institut de Recherche pour le Développement (IRD).
Detalles Bibliográficos
Autores: Aguirre Alegre, Enoch Matthew, Benavente Escobar, Carlos Lenin, Rosell Guevara, Lorena Nicole, García Fernández Baca, Briant, Taipe Maquerhua, Edu Luis
Formato: objeto de conferencia
Fecha de Publicación:2019
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/2599
Enlace del recurso:https://hdl.handle.net/20.500.12544/2599
Nivel de acceso:acceso abierto
Materia:Paleosismología
Tectónica
Terremotos
Sismos
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dc.title.es_PE.fl_str_mv Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
title Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
spellingShingle Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
Aguirre Alegre, Enoch Matthew
Paleosismología
Tectónica
Terremotos
Sismos
title_short Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
title_full Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
title_fullStr Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
title_full_unstemmed Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
title_sort Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century
author Aguirre Alegre, Enoch Matthew
author_facet Aguirre Alegre, Enoch Matthew
Benavente Escobar, Carlos Lenin
Rosell Guevara, Lorena Nicole
García Fernández Baca, Briant
Taipe Maquerhua, Edu Luis
author_role author
author2 Benavente Escobar, Carlos Lenin
Rosell Guevara, Lorena Nicole
García Fernández Baca, Briant
Taipe Maquerhua, Edu Luis
author2_role author
author
author
author
dc.contributor.author.fl_str_mv Aguirre Alegre, Enoch Matthew
Benavente Escobar, Carlos Lenin
Rosell Guevara, Lorena Nicole
García Fernández Baca, Briant
Taipe Maquerhua, Edu Luis
dc.subject.es_PE.fl_str_mv Paleosismología
Tectónica
Terremotos
Sismos
topic Paleosismología
Tectónica
Terremotos
Sismos
description Trabajo presentado en el 8th International Symposium on Andean Geodynamics (ISAG), realizado en Quito-Ecuador, del 24-26 setiembre, 2019. Evento organizado por el Instituto Geofísico, Escuela Politécnica Nacional (IG-EPN) del Ecuador, y el French Institut de Recherche pour le Développement (IRD).
publishDate 2019
dc.date.accessioned.none.fl_str_mv 2020-05-18T06:53:56Z
dc.date.available.none.fl_str_mv 2020-05-18T06:53:56Z
dc.date.issued.fl_str_mv 2019-09
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dc.identifier.citation.es_PE.fl_str_mv Aguirre, E.; Benavente, C.; Rosell, L.; García, B. & Taipe, E. (2019). Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century [Abstract]. Trabajo presentado en el 8th International Symposium on Andean Geodynamics (ISAG), Quito-Ecuador, 24-26 setiembre, 2019. 1 p.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/2599
identifier_str_mv Aguirre, E.; Benavente, C.; Rosell, L.; García, B. & Taipe, E. (2019). Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century [Abstract]. Trabajo presentado en el 8th International Symposium on Andean Geodynamics (ISAG), Quito-Ecuador, 24-26 setiembre, 2019. 1 p.
url https://hdl.handle.net/20.500.12544/2599
dc.language.iso.es_PE.fl_str_mv eng
language eng
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dc.coverage.spatial.es_PE.fl_str_mv Perú
dc.publisher.es_PE.fl_str_mv 8th International Symposium on Andean Geodynamics (ISAG)
dc.publisher.country.es_PE.fl_str_mv EC
dc.source.es_PE.fl_str_mv Instituto Geológico, Minero y Metalúrgico – INGEMMET
Repositorio Institucional INGEMMET
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spelling Aguirre Alegre, Enoch MatthewBenavente Escobar, Carlos LeninRosell Guevara, Lorena NicoleGarcía Fernández Baca, BriantTaipe Maquerhua, Edu LuisPerú2020-05-18T06:53:56Z2020-05-18T06:53:56Z2019-09Aguirre, E.; Benavente, C.; Rosell, L.; García, B. & Taipe, E. (2019). Active faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th century [Abstract]. Trabajo presentado en el 8th International Symposium on Andean Geodynamics (ISAG), Quito-Ecuador, 24-26 setiembre, 2019. 1 p.https://hdl.handle.net/20.500.12544/2599Trabajo presentado en el 8th International Symposium on Andean Geodynamics (ISAG), realizado en Quito-Ecuador, del 24-26 setiembre, 2019. Evento organizado por el Instituto Geofísico, Escuela Politécnica Nacional (IG-EPN) del Ecuador, y el French Institut de Recherche pour le Développement (IRD).Subduction earthquakes are considered the main source for seismic hazard in Peru (Villegas-Lanza et al., 2016). However, in recent years, it has been made an effort to generate a database of active faults for southern Peru (Benavente Carlos et al., 2017, Benavente et al., 2018), to propose these as a potential danger. In this way, we carried out morpho-structural and paleoseismological analyzes to get data for use it in empirical relationships and propose the magnitude of a potential earthquake. The Purgatorio Mirave fault (PMF) is located at forearc of southern Peru. Benavente et al. (2017) propose its activity in the last 6 ka, through TCN (Be10) dating over the fault scarps. In order to reconstruct the deformation and seismic history of PMF, we carried out studies of paleoseismology. Before the excavation of paleosismological trench, we acquired high resolution DEM and imagery with LIDAR and drone with the purpose to do a detailed mapping of all segments associated to PMF and to identify favorable areas for morpho-structural and paleosismological analyzes. With these, we determine 200km of superficial ruptures, that are distributed inside an area of 70 km for length and 2 km for width. The high resolution images (5cm x pixel) shows sub-parallel segments, forming sigmoidal structures, in echelons, pop-up and pressure ridges. The trench was excavated at the bottom of a valley (near the town of Mirave-Tacna), where there is a 2-meter-high fault scarp, that is affecting unconsolidated alluvial deposits. The trench (5 m long and 4 m deep) shows a reverse fault that places Oligocene rocks (Fm. Moquegua) over Holocene deposits. We identified two colluvial wedge, which are dated in 15 191-14 690 cal BC and 1668-1787 cal AD by radiocarbon C14. The most recent event generated a vertical rupture of 0.90 m. According to our results (rupture length and vertical displacement of the PMF) and using the scale proposed by Wells and Coppersmith (1994), we determine a magnitude of 7.5Mw for the last event. In this sense, between the end of 18th and the beginning of 19th century, in southern Peru important geological processes were registered: a) A large cortical earthquake associated with the reactivation of the PMF, and b) The explosive eruption of the Tutupaca volcano (Samaniego et al., 2015), located 30 km from the PMF.application/pdfeng8th International Symposium on Andean Geodynamics (ISAG)ECinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/deed.esInstituto Geológico, Minero y Metalúrgico – INGEMMETRepositorio Institucional INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETPaleosismologíaTectónicaTerremotosSismosActive faulting, paleoseismology and seismic hazard in forearc of southern Peru: First evidence of a crustal earthquake in the 19th centuryinfo:eu-repo/semantics/conferenceObjectGeologíaORIGINALAguirre-Active_faulting_paleoseismology.pdfAguirre-Active_faulting_paleoseismology.pdfArtículo de congresoapplication/pdf358887https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2599/1/Aguirre-Active_faulting_paleoseismology.pdf56b7edc300a030ecf3c0b74b68cbb718MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2599/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52TEXTAguirre-Active_faulting_paleoseismology.pdf.txtAguirre-Active_faulting_paleoseismology.pdf.txtExtracted texttext/plain2777https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2599/3/Aguirre-Active_faulting_paleoseismology.pdf.txt008ba5492994456294830def2d6e6c7bMD53THUMBNAILAguirre-Active_faulting_paleoseismology.pdf.jpgAguirre-Active_faulting_paleoseismology.pdf.jpgGenerated Thumbnailimage/jpeg21362https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2599/4/Aguirre-Active_faulting_paleoseismology.pdf.jpg67ce1982f2938b3931161505ea39edddMD5420.500.12544/2599oai:repositorio.ingemmet.gob.pe:20.500.12544/25992020-10-14 18:54:54.866Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.peTGljZW5jaWEgZGUgVXNvCgpFbCBJbnN0aXR1dG8gR2VvbMOzZ2ljbywgTWluZXJvIHkgTWV0YWzDunJnaWNvIOKAkyBJTkdFTU1FVCwgZGlmdW5kZSBtZWRpYW50ZSBzdSByZXBvc2l0b3JpbyBsYSBwcm9kdWNjacOzbiBjaWVudMOtZmljYSB5IHTDqWNuaWNhIHByb2R1Y2lkYSBwb3IgbG9zIG1pZW1icm9zIGRlIGxhIGluc3RpdHVjacOzbi4gRWwgY29udGVuaWRvIGRlIGxvcyBkb2N1bWVudG9zIGRpZ2l0YWxlcyBlcyBkZSBhY2Nlc28gYWJpZXJ0byBwYXJhIHRvZGEgcGVyc29uYSBpbnRlcmVzYWRhLgoKU2UgYWNlcHRhIGxhIGRpZnVzacOzbiBww7pibGljYSBkZSBsYSBvYnJhLCBzdSBjb3BpYSB5IHJlcHJvZHVjacOzbi4gUGFyYSBlbGxvIGVzIG5lY2VzYXJpbyBxdWUgc2UgY3VtcGxhIGNvbiBsYXMgc2lndWllbnRlcyBjb25kaWNpb25lczoKLSBFbCBuZWNlc2FyaW8gcmVjb25vY2ltaWVudG8gZGUgbGEgYXV0b3LDrWEgZGUgbGEgb2JyYSwgaWRlbnRpZmljYW5kbyBvcG9ydHVuYSB5IGNvcnJlY3RhbWVudGUgYSBsYSBwZXJzb25hIHF1ZSBwb3NlYSBsb3MgZGVyZWNob3MgZGUgYXV0b3IuCi0gTm8gZXN0w6EgcGVybWl0aWRvIGVsIHVzbyBpbmRlYmlkbyBkZSBsYSBvYnJhIGNvbiBmaW5lcyBkZSBsdWNybyBvIGN1YWxxdWllciB0aXBvIGRlIGFjdGl2aWRhZCBxdWUgcHJvZHV6Y2EgZ2FuYW5jaWFzIGEgbGFzIHBlcnNvbmFzIHF1ZSBsbyBkaWZ1bmRlbiBzaW4gZWwgY29uc2VudGltaWVudG8gZGVsIGF1dG9yLgotIExvcyB0cmFiYWpvcyBxdWUgc2UgcHJvZHV6Y2FuIGEgcGFydGlyIGRlIGxhIG9icmEgZGViZW4gcG9zZWVyIGxhIGNpdGFjacOzbiBwZXJ0aW5lbnRlIGRlIGFjdWVyZG8gYSBjdWFscXVpZXJhIGRlIGxvcyBlc3RpbG9zIChBUEEsIElTTywgVmFuY3V2ZXIsIGV0YykgZWxlZ2lkb3MgcGFyYSBsYSByZWRhY2Npw7NuIGRlIGxhcyByZWZlcmVuY2lhcyBiaWJsaW9ncsOhZmljYXMuIENhc28gY29udHJhcmlvIHNlIGluY3Vycmlyw6EgZW4gbGEgZmlndXJhIGp1csOtZGljYSBkZWwgcGxhZ2lvLgoKTG9zIGRlcmVjaG9zIG1vcmFsZXMgZGVsIGF1dG9yIG5vIHNvbiBhZmVjdGFkb3MgcG9yIGxhIHByZXNlbnRlIGxpY2VuY2lhIGRlIHVzby4KCkRlcmVjaG9zIGRlIGF1dG9yCgpMb3MgZGVyZWNob3MgZGUgYXV0b3Igc2UgZW5jdWVudHJhbiBwcm90ZWdpZG9zIHBvciBsYSBsZWdpc2xhY2nDs24gcGVydWFuYTogTGV5IHNvYnJlIGVsIERlcmVjaG8gZGUgQXV0b3IgcHJvbXVsZ2FkbyBlbiAxOTk2IChELkwuIE7CsCA4MjIpLCBMZXkgcXVlIG1vZGlmaWNhIGxvcyBhcnTDrWN1bG9zIDE4OMKweSAxODnCsCBkZWwgZGVjcmV0byBsZWdpc2xhdGl2byBOwrAgODIyLCBMZXkgc29icmUgRGVyZWNob3MgZGUgQXV0b3IgcHJvbXVsZ2FkYSBlbiAyMDA1IChMZXkgTsKwIDI4NTE3KSwgRGVjcmV0byBMZWdpc2xhdGl2byBxdWUgYXBydWViYSBsYSBtb2RpZmljYWNpw7NuIGRlbCBEZWNyZXRvIExlZ2lzbGF0aXZvIE7CsCA4MjIsIExleSBzb2JyZSBlbCBEZXJlY2hvIGRlIEF1dG9yIHByb211bGdhZG8gZW4gMjAwOCAoRC5MLiBOwrAgMTA3NikuCg==
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