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Geological data on slip rates of active faults indicate that significant E W contraction across the NE Japan arc occurs on different time scales (Wesnousky et al. 1982).
These faults indicate that a high-throughput diagnostic methods with good specificity and sensitivity is necessary.
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Stratigraphic growth across the faults indicates that main fault activity occurred during the Plio-Pleistocene, which corresponds to the timing of tectonic loading on Timor Island and the development of lithospheric flexure.
There is no evidence for growth faulting along these sediment-restricted faults, indicating that the fault system is young.
Seismic images of sediments deposited in an ancient lake overlying the southern end of the fault indicate that episodic flooding may have triggered earthquakes in the past.
The relatively large distances between their hypocenters and the mainshock fault indicate that they do not relate to the mainshock event.
However, the displacements are mainly concentrated on the west side of the fault, indicating that the fault is dipping to the west.
Two clusters included more than ten events and occurred some distance from the mainshock fault, indicating that the clusters did not relate to the mainshock event.
A digital map of the active fault indicates that several faults are located in this area (Nakata and Imaizumi 2002), and a high phase gradient was obtained along the faults.
This activity starts near the 60-km-depth contour of the subduction earthquakes and becomes shallower toward the Sagaing Fault, indicating that this fault is located where the cut-off depth of the seismicity becomes shallower.
Second, secondary hydrous minerals were observed in the drill core that penetrated the active segment of the fault, indicating that aqueous fluids were present in the zone at some time in the recent past.
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