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We investigate the relationship of permeability of fault developing in Neogene mudstone layer with mechanical properties of the host rock and stress condition (or depth) at the faulting, focusing on the Wakkanai Formation (middle to late Miocene, siliceous mudstone) and the Koetoi Formation (late Miocene to Pliocene, diatomaceous mudstone) at the Horonobe area, northern Hokkaido. Based on the previous...
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