The clearance of a DC fault needs to be coordinated in both the fast DC breakers stationed at the inverter state and the AC breakers stationed at the rectifier state.
Understanding further the nature and evolution at lithospheric scale of the Sea of Marmara on the North Anatolian Fault needs constraints on the deep crustal and Moho spatial variation.
Douglas Wiens, a professor of earth and planetary sciences, reported: "The strongest earthquakes in the last few years have come from the Wabash Valley Fault", and said the fault needs more scientific observation.
She was literal-minded well beyond a fault, needed jokes explained to her at length, and could be relied on to grasp the wrong end of any proffered stick, and had, as one of her ministers said, the habit of "jumping the rails" in conversation.
The results show that in order to detect a shift in the mean or a shift in the variance, the GLR charts designed to detect either type of fault need to be implemented in parallel as they provide lower missed detection rates, than a GLR chart designed to detect shift in both the process mean and variance simultaneously.
However, the magnitude of the vertical ground displacement across the normal fault needed to induce fracture varies considerably for the different burial conditions that were considered, and the rotation angle increases steadily after fracture if the amount of vertical ground displacement continues to grow.
When asked how far away the Hollywood fault needed to be to require a fault investigation, Zamperini did not specify.
To enable non-experts in vibration analysis to perform condition monitoring, the overhead of feature engineering for specific faults needs to be reduced as much as possible.
Therefore, these faults need to be kept within the allowable level through an investigation of their effects on the interactions between the train and track.
In fault diagnosis system designers or engineers should analyse systems in order to define their input patterns, features, classes required for pattern recognition, and corresponding residuals, fault symptoms, faults needed for fault diagnosis, respectively.
We nevertheless caution that the calculation idealizes stress transfer because smaller faults need not share the same geometry as the major faults sampled here, and the dip and rake of even major faults are often poorly known.
