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While these variations do well with Stampe-type objections (because it is not the purpose of a belief that one is going to double fault to cause a double fault), they nonetheless would seem to be subject to objections by those who think that beliefs in the good can also perform their functions by moving one to act.
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Since they were not able to reproduce the observed thermal anomalies in the western Molasse Basin with such a conductive approach, they presumed fluid flow along E W striking faults to cause temperature differences of more than 10 K in the basin.
It was discovered that the quake might have been caused by reservoir-induced seismicity, i.e. the weight of the water from Lake Oroville, whose dam had been completed in 1968, was pressing down on the fault zone enough to cause geologic stress, upon which the fault might slip and cause an earthquake.
Thus the fault area likely to cause CF can be identified.
The fault area likely to cause concurrent CF in multi-infeed HVDC systems is the intersection of the CF-sensitive areas of different HVDC systems.
Shear localization in foliated, phyllosilicate-rich fault rocks is known to cause weakening in crustal fault zones (e.g., Stewart et al. 2000; Imber et al. 2001; Gueydan et al. 2003; Collettini and Holdsworth 2004; Wibberley and Shimamoto 2005; Jefferies et al. 2006).
The fault model comprises transient faults that are unable to cause permanent failure of a system.
Therefore, the fracture zone associated with the MTL fault system has possibility to cause increase in attenuation coefficients in the field data case (Fig. 8c).
The magnitude of the maximum horizontal stress (Shmax) is constrained by assuming that the ratio of the maximum to minimum effective stress cannot exceed that required to cause faulting on an optimally oriented pre-existing fault (Sibson 1974).
These variations in geological setting along the strike of the Yamasaki fault system are expected to cause variations in resistivity structure.
The mega-splay fault is branching fault that have the potential to cause large coseismic slip (e.g., Fukao 1979).
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