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Fossil imbricate thrusts, branching from a décollement in an ancient accretionary prism (the Miura–Boso accretionary prism), are exposed in the southern parts of the Miura and Boso peninsulas in central Japan. An analysis of the clay mineralogy of fault rocks along one of the imbricate thrust faults, the Shirako Fault, revealed local illitization of mixed-layer illite–smectite (I–S) and the partial...
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