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The Philippine Sea Plate is subducting in the NW direction beneath the Eurasian Plate.
Flow direction evidenced by AMS gives an overall NW direction for the flow.
However, during Pleistocene, these saline waters became exchanged with fresh water from the NW direction.
However, most of the fractured bedrock were found localised within the SE region and aligned in NW direction, while other fractured zones are widely spaced from one another.
At the western side of Ichinoike (NW direction), the PDC ran ~1.5 km down a slope of ~18° from an altitude of ~2900 m.
The GPS stations were found to displace in the NW direction uniformly with the magnitude slowly decreasing with increasing distance from the fault.
Similar(43)
Of the 66 juveniles at downwind distances, 18%, 48%, and 33% of them were found in SW, W, and NW directions, respectively.
They trend in a N-NW direction, corresponding to the extension of the northern section of the Huya Fault.
The slope, oriented approximately along the SE-NW direction (with a dip of about 30 38°) is mainly made of Maiolica Formation which consists of well stratified micritic limestone (from 10 cm to 1 m) with intercalation of thin clay layers.
Both the 2H and 4H unit cells are elongated in the NW growth direction and contracted in the radial direction compared to 3C.
Moreover, the carriers inside the substrate distribute relatively even in the NW radial direction while gradually fall off along the longitudinal direction.
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