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The slip on the Futagawa fault is mainly strike slip.
Top: major earthquakes with right-lateral strike slip from 2006 to 2008.
The second row reports interferograms relative to strike slip faults.
During Quaternary period many dip and strike slip faults ocurred in the area.
Results demonstrated that the coseismic slip was mainly dominated by strike slip.
We calculated this term for strike slip and dip slip, respectively.
The central part surrounding Lake Suwa forms a strike slip fault (e.g., Fujimori, 1991).
The M6.5 and M7.3 events were characterized by strike slip and normal faults, respectively.
We assume a two-dimensional vertical fault with right-lateral strike slip.
A strike slip stress field in which intermediate principal stress is vertical is assumed here.
Red indicates normal faulting, green indicates strike slip, and blue indicates thrust faulting.
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