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Proceedings of the Ocean Drilling Program, 131 Scientific Results
Complete penetration of frontal thrust and décollement of the Nankai Trough accretionary complex in Site 808 during ODP Leg 131 provided a wealth of structural observations and physical property data. In this paper possible mechanisms are discussed that could be responsible for the development of irregular downhole trends in acoustic anisotropy observed in Site 808. After various steps of data reduction and screening, a paleomagnetic reorientation procedure is applied to a selected group ofdoi:10.2973/odp.proc.sr.131.121.1993 fatcat:jqqendih6jgl7jpki644f6ulwy