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Volumn 466, Issue 3-4, 2009, Pages 255-267

Subducting oceanic high causes compressional faulting in southernmost Ryukyu forearc as revealed by hypocentral determinations of earthquakes and reflection/refraction seismic data

Author keywords

Earthquake location; Ryukyu subduction; Splay fault; Taiwan

Indexed keywords

3D VELOCITIES; ACTIVE FAULTS; ACTIVE SEISMIC; COMPRESSIONAL; EARTHQUAKE LOCATION; FOCAL MECHANISMS; FOREARC; HYPOCENTER LOCATIONS; OCEANIC CRUSTS; REVERSE FAULTING; REVERSE FAULTS; RYUKYU SUBDUCTION; SEDIMENTOLOGICAL DATUM; SEISMIC DATUM; SEISMIC LINES; SPLAY FAULT; SUBDUCTION INTERFACES; SUBDUCTION ZONES; TAIWAN;

EID: 60949104283     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2007.11.018     Document Type: Article
Times cited : (19)

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