S-Local-Wave Seismic Anisotropy in the Forearc Above the Subducted Nazca Plate Between 33°S and 34.5°S

S-wave splitting from local earthquakes within the Nazca plate that are deeper than the interplate seismogenic zone enabled the determination of the fast velocity direction, Φ, and the lag time, δt, in the forearc of the overriding plate. Data were collected from 20 seismic stations, most of which w...

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Publicado: 2016
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00334553_v173_n4_p1143_Nacif
http://hdl.handle.net/20.500.12110/paper_00334553_v173_n4_p1143_Nacif
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