Three-dimensional P-wave velocity structure on the shallow part of the Central Costa Rican Pacific margin from local earthquake tomography using off- and onshore networks

Geophysical Journal International

Volumn 179, Issue 2, 2009, Pages 827-849

  Arroyo, I G ^a   Husen, S ^b   Flueh, E R ^a   Gossler, J ^a   Kissling, E ^b   Alvarado, G E ^c  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b ETH ZURICH   (Switzerland)

^c UNIVERSIDAD DE COSTA RICA   (Costa Rica)

Author keywords

Continental margins: convergent; Crustal structure; Seismic tomography; Subduction zone processes

Indexed keywords

CONTINENTAL MARGIN; CONVERGENT MARGIN; CRUSTAL STRUCTURE; EARTHQUAKE MAGNITUDE; FOREARC BASIN; OCEANIC CRUST; P-WAVE; SEAFLOOR; SEISMIC TOMOGRAPHY; SEISMICITY; SEISMOLOGY; SEISMOTECTONICS; SUBDUCTION ZONE; THREE-DIMENSIONAL MODELING; UNDERPLATING; UPLIFT; UPPER CRUST; VELOCITY STRUCTURE;

CENTRAL AMERICA; COSTA RICA;

EID: 70350417006     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2009.04342.x     Document Type: Article

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