Updip limit of the seismogenic zone beneath the accretionary prism of Southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress

Geology

Volumn 29, Issue 2, 2001, Pages 183-186

  Moore, J C ^a   Saffer, D ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Accretionary prism; Diagenesis; Faults; Fluid pressure; Subduction zone

Indexed keywords

CEMENTING (SHAFTS); CLAY MINERALS; EARTHQUAKES; PRISMS; SEISMOGRAPHS; ZEOLITES;

ACCRETIONARY PRISM; CO-SEISMIC DISPLACEMENT; DIAGENESIS; FLUID PRESSURES; LOW-GRADE METAMORPHIC; QUARTZ CEMENTATION; SUBDUCTION ZONES; VELOCITY-WEAKENING;

FAULTING;

ACCRETIONARY PRISM; DIAGENESIS; EARTHQUAKE; FLUID PRESSURE; LOW GRADE METAMORPHISM; SEISMICITY; SUBDUCTION ZONE;

JAPAN; NANKAI TROUGH; PACIFIC OCEAN; SHIMANTO BELT;

EID: 84879884609     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2001)029<0183:ULOTSZ>2.0.CO;2     Document Type: Article

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