Pn-wave observations in Costa Rica

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Autor principal: Ota Kulhánek
Formato: Artículo científico
Lenguaje:en
Publicado: Universidad Nacional Autónoma de México 1998
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author Ota Kulhánek
author_facet Ota Kulhánek
contents Pn-wave observations in Costa Rica Ota Kulhánek Ronnie Quintero Ciencias de la Tierra Vp Time Vs ratio anisotropy Costa Rica P- and S-wave arrival-time data from 100 local and regional earthquakes recorded by the OVSICORI-UNA Costa Rica seismographicnetwork, between 1984 to1990, are employed to extract crustal and upper mantle information beneath Costa Rica. Pn-wavevelocity, Poisson’s ratio, velocity anisotropy and station corrections were calculated in this study. Poisson’s ratio for the uppermostmantle beneath Costa Rica is 0.265 and the Pn velocity is 7.81 km/sec. The present study does not reveal any significant Pn velocityanisotropy. The computed Moho depth beneath Costa Rica is approximately 34 km. 1998 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56837303 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.3 Vol.37
format Artículo científico
id redalyc_56837303
institution Redalyc
language en
publishDate 1998
publisher Universidad Nacional Autónoma de México
spellingShingle Pn-wave observations in Costa Rica
Ota Kulhánek
Ciencias de la Tierra
Vp
Time
Vs ratio
anisotropy
Costa Rica
Pn-wave observations in Costa Rica Ota Kulhánek Ronnie Quintero Ciencias de la Tierra Vp Time Vs ratio anisotropy Costa Rica P- and S-wave arrival-time data from 100 local and regional earthquakes recorded by the OVSICORI-UNA Costa Rica seismographicnetwork, between 1984 to1990, are employed to extract crustal and upper mantle information beneath Costa Rica. Pn-wavevelocity, Poisson’s ratio, velocity anisotropy and station corrections were calculated in this study. Poisson’s ratio for the uppermostmantle beneath Costa Rica is 0.265 and the Pn velocity is 7.81 km/sec. The present study does not reveal any significant Pn velocityanisotropy. The computed Moho depth beneath Costa Rica is approximately 34 km. 1998 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56837303 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.3 Vol.37
title Pn-wave observations in Costa Rica
topic Ciencias de la Tierra
Vp
Time
Vs ratio
anisotropy
Costa Rica
url https://www.redalyc.org/articulo.oa?id=56837303