It should be noted that the simulated faults are located in PGB 1.
Those faults are located in the Lesser Himalaya on the hanging side of the HFT.
This could happen where the geological faults are located and influence the geometric arrangement.
One of the more conspicuous of these faults is located at a depth of 138.5 m in Hole 1.
The distances in Table 1 show where the faults are located with respect to the R A relay.
Whereas weak faults are located mostly in the SE, major faults, particularly two that cut through the Edwards into the Austin Chalk, are located in the NW.
Top depth of all faults is located at surface Fig. 5 Comparison with observation of pixel-offset data, calculation from slip distribution and residual.
Large active volcanoes, such as Mt. Aso and Kuju, are located within this graben, and major active faults, such as the Beppu–Haneyama, Futagawa, and Hinagu faults, are located in or along the edges of this graben.
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.
The closest profile to the 1896 Sanriku earthquake source (Fig. 6) indicates that both faults are located at the contact zone between deformed area (Vp = 3.2 2.6 km/s) and oceanic crust (Vp = 5.3 5.6 km/s), suggesting similarities of fault zone properties.
However, as the majority of plate boundary faults are located in smectite-rich horizons (Underwood 2007), the S-I reaction could also supply significant amounts of silica, although this factor has not been assessed in previous research.
