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The Nobeoka Thrust, an ancient megasplay fault in the Shimanto Belt, southwestern Japan, contains fault rocks from the seismogenic zone, providing an accessible analog of active megasplay faults in deep subduction settings. In this study, the paleostress along the Nobeoka Thrust was analyzed using multiple inversion techniques, including k‐means clustering of fault datasets acquired from drillcores...
An ancient subduction thrust, developed at the top of oceanic basaltic crust, is exposed in the Shimanto accretionary complex of eastern Shikoku, southwest Japan. The fault zone structure indicates that slip was localized along a few centimeters-thick layer in which fluidization of comminuted material is recorded. To identify possible clay mineral reactions during frictional heating along subduction...
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