Exact(3)
The GF consists of several subsidiary fracture zones surrounding the main fault, which were identified by individual FCZs.
This anomaly can be considered as FZC of the main fault, which has a width of ~700 m and extends to a depth of ~300 m.
According to the seismic survey, they pointed out that the EBFZNP, recognized on the surface, is a west-dipping reverse fault that is a secondary fault derived from the east-dipping main fault, which extends below the Echigo Mountains.
Similar(57)
Firstly, the fault observer was brought in to observe the trend of the collective angle of blade resulted by the main faults, which can produce control signals according to the fault signals; And then in order to compensate the interference and the model dynamics errors, the adaptive back-stepping sliding mode controller was designed, the control laws were also given.
Down in the jungle in central southern Nepal, Bollinger's team dug trenches across the country's main earthquake fault (which runs for more than 1,000km from west to east), at the place where the fault meets the surface, and used fragments of charcoal buried within the fault to carbon-date when the fault had last moved.
The fault-growth curves allowed us to divide the faulted rift border into four main fault systems, which provide roughly similar Dmax/L ratios.
This damage zone is located on the southern side of the fault and defines an asymmetry around the main fault strand, which demonstrates distributed conduit behavior of fluid flow.
The proposed multi-functional DVR control strategy is applied to a three-phase fault which is the main cause of the worst voltage sag.
Geologically, the hydroelectric installation is located in the Higher Himalayan Crystalline, just above the active Karcham Normal Fault, which is reactivating the Early Miocene Main Central Thrust, one of the principal Himalayan faults.
3. Zone A corresponds to the southern part of Hinagu fault, which is 10 50 km from the hypocenter of the main shock.
A Mw 6.0 aftershock approximately 1 minute after the main event is inferred to have ruptured an updip region of the mainshock fault which is relatively devoid of small aftershock seismicity.
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