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The evaporite eruptions related to the presence of weak tectonic nodules were conditioned from the intersection of the cross fault with longitudinal faults.
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These loops belong to the intersecting places of transverse and longitudinal fault generated since the rifting phase (T3-Cr1).
These loops belong to the intersection of the transverse and longitudinal fault generated since the rifting phase (T3 to J3-Cr1).
(4) Middle Miocene basin morphology in central Hokkaido was successfully reproduced by assuming hybrid fault motions; these included initially right-lateral and subsequently reverse motions in the longitudinal fault zone.
CHF Changhua fault, CLPF Chelungpu fault, STF Shuangtung fault, LVF Longitudinal Valley fault Table 1 Earthquake parameters for the target events and EGF events determined by CWB No. Date (UT) Long.
In addition, in the early compression stage (Cr2-Serravalian), longitudinal listric faults started to react by passing into thrusting faults.
During the rifting stage (T3-Cr1), the Berati anticlinal belt was divided into many horsts and grabens due to transverse and longitudinal listric faults (Fig. 14).
The Chihshang and Rueisuei ruptures are along segments of the Longitudinal Valley fault, a left-lateral oblique fault along which the Coastal Range thrusts westward over the Longitudinal Valley.
The deformation along the LV is mostly accommodated by two large structures: the Longitudinal Valley fault (LVF) and the Central Range fault (CRF).
Longitudinal Valley Fault, H.B. Huatung Basin, G.R. Gagua Ridge, L.V.A. Luzon Volcanic Arc, L.O.F.Z.
Numerical modeling demonstrated that dextral slip on a bunch of longitudinal strike-slip faults restored the Neogenedepocenters in central Hokkaido, together with an east-west compressive regime related to an arc-arc collision.
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