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At the Jigokudani valley (SW direction), the PDC travelled ~2.4 km down a slope of ~22°.
Scouring features can also be clearly observed along the SW direction, including scour depressions and linear sandy remnants.
Thereafter, the polarity aligned with the crack opening, i.e., a tilt downward in the SW direction at the KZR station.
The distant current sheet extends anti-sunward and follows the randomly changing SW direction in a windsock-like manner.
In addition, the variable head boundary between −16 and −22 m asl is assigned in SW direction.
After the main shock, the epicenters of aftershocks migrated from Kumamoto in NE and SW direction (Fig. 1).
Similar(48)
The T axes indicate that the Denizli Graben is opening in the NE-SW direction.
The third set, trending in the NE-SW direction, are considered as strike-slip faults.
Previous studies pointed out that the rift is an asymmetrical half-graben elongated along the NE-SW direction.
The third set represents a group of strike-slip faults trending mainly towards the NE-SW direction.
The focal mechanisms reflect that the extensional regime is dominant in the NE-SW direction in the Denizli Graben.
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