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The scheme is designed to detect the fault, estimate the faulted side, classify the fault type and identify the faulted phase.
The transient traveling wave is mostly used in protection to determine the faulted line and the fault location.
The FDS basic objectives are mainly: (1) the detection of the system fault; (2) the localization of the faulted zone; (3) the classification of the fault type; and finally (4) the identification of the faulted phase.
The fault-growth curves allowed us to divide the faulted rift border into four main fault systems, which provide roughly similar Dmax/L ratios.
The dashed curves emanating from the pre-fault equilibrium are the six fault-on trajectories without tripping the faulted lines.
Besides, the faulted phase as well as fault type detection has been suggested in this paper using same measurements.
Recurrent seismicity provides eloquent testimony to the neotectonic resurgence of the faulted terrains and the terrane-defining faults.
During normal fault development, fault propagation folds are formed to accommodate the variation of the displacement between the faulted beds and the unfaulted beds above the fault tips.
It delineates a single step method to find out the faulted line and the exact location of fault.
Although the input signals and discrimination methods of these protection algorithms are different, all algorithms essentially use fault initiated travelling waves to discriminate the faulted line.
Accurate information about the faulted line or cable section expedites system restoration following the fault occurrence.
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