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Caltech geologist Kerry Sieh explained to reporters why scientists were uncertain which fault blew.
Then node voltages at substation can be expressed as a product of bus impedance matrix and current injection at substation, from which fault location can be estimated.
Model-based fault detection and isolation (FDI) requires an analytical system model from which fault indicators can be derived by assigning proper computational causalities.
To solve the conflicts and reduce incorrect diagnosis results, an amendment based on D-S theory determined which fault contributed more to causing the corresponding symptoms.
However, for incipient faults in which fault steadily progresses over time and there is a changeover from normal operation to faulty operation, using discrete decision function does not reveal any evidence about the progress and depth of the fault.
The method is shown to be optimal for detection in the Neyman-Pearson sense, it returns an envelope spectrum comparable to the best that can be obtained by other means – which often require a careful pre-filtering step – from which fault frequencies can be identified, and it eventually returns the fault signal from which subsequent severity/health indicators can be computed.
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The architecture of the sequences in the different structural belts of the depression is complicated by the relationship between the rate at which fault-controlled accommodation was created and the rate of sediment supply.
Cataclastite, any rock produced by dynamic metamorphism during which faulting, granulation, and flowage may occur in previously crystalline parent rocks.
When combined with information about the faults present in a given area, the scientists were able to assess which faults are likely to be problematic and why.
We use the finite element (FE) method to examine which faults are activated and how the surrounding material responds for both elastic and elastic plastic off-fault descriptions.
Students and faculty study the mechanics of fault rupture and the physical mechanisms by which faults and fractures generate seismic waves.
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