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From the comparison with tomographic studies we interpret that both strike-slip events apart from the Atotsugawa fault and normal faulting events in the central section of fault imply the effect of crustal fluids to the stress field.
When pressure is building in a section of fault, Dr. Thatcher said, it will warp the surface in a characteristic way that reveals the location and depth of these areas where pressures are bottled up.
The series of earthquakes, including the latest aftershock, are "like ants chewing around the edges" of a 240-mile-long section of fault off Padang that is overdue for a great earthquake the likes of which has not occurred along that part of the coast since 1833.
Over the years, these observations have helped seismologists anticipate another magnitude-8 quake on this section of fault off central Chile, where the Nazca tectonic plate dives beneath South America.
It will also collect more data especially from a critical offshore section of fault ruptured by the quake and provide day-to-day advice to assist relief and recovery efforts.
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In Section Implementation of fault detection and isolation we concentrate on the implementation of the router and describe how the means of fault detection and isolation are realized.
An experiment is defined by experiment parameters that consist of the router configuration (see Section Implementation of fault detection and isolation, Listing 1) for the CISes and CAN traffic patterns for each CTN.
"Locked" sections of faults, meanwhile, are the ones we generally worry about, gathering stress over decades or centuries, and building strain to be released in a catastrophic earthquake someday. .
The 543 Fault that developed near the 527 Fault is a secondary normal fault, with nearly concordant strike and dip to that of the eastern section of 527 Fault (Fig. 3).
The historical earthquake catalog of the Huya Fault shows three moderately strong earthquakes occurred in the southern section of the fault during 1976 and completely ruptured to the surface.
The western section of 527 Fault in the Liudong area was very active in the main rift I stage, causing strong normal faulting throughout this area and forming a steep slope fault belt.
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