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PERMEABILITY AND STRENGTH OF CORE SAMPLES FROM THE NOJIMAFAULT OF THE 1995 KOBE EARTHQUAKE (2000)

The 1995 Hyogoken-Nanbu (Kobe) earthquake, M=7.2, ruptured the Nojima fault. We have studied core samples taken from two scientific drillholes which crossed the fault zone in the epicentral region on Awagi island.

Reference:
"Proceedings of the International Workshop on the Nojima Fault Core and Borehole Analysis, USGS Open-file Report 00-129
Organization:
US Geological Survey
Japan, Kobe
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