泥質片岩の延性度較差:地震波のブライトスポットに関する構造岩石学的根拠
Ductility contrast in pelitic schist: microtectonic evidence for seismic bright spots

Tayyaba Mateen, Hiroshi Yamamoto, Hafiz Rehman
2014 Annual Meeting of the Geological Society of Japan  
This study presents geological evidence supporting the existence of 'seismically bright layer ' (Terabayashi et al., 2010) as sub-crustal over-pressured silicic fluids. According to the present study of Iwakuni area, SW Japan we hypothesize that seismic bright-spot reflections (e.g. Ito, 1999) may be caused by a
doi:10.14863/geosocabst.2014.0_025 fatcat:daptdqupeneb7aysmccwj6pdxu