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fault symptom - translation to russian
SMALL STEP OR OFFSET ON THE GROUND SURFACE WHERE ONE SIDE OF A FAULT HAS MOVED VERTICALLY WITH RESPECT TO THE OTHER
Fault Scarp; Fault escarpment
fault symptom
общая лексика
признак неисправности
line-to-ground fault
ABNORMAL ELECTRIC CURRENT
Asymmetric fault; Symmetric fault; Transient fault; Persistent fault; Fault current; Electrical faults; Prospective fault current; Earth fault; Restricted earth fault; Fault (electric); Ground Fault; Ground fault; SLGF; Single line to ground fault; Line to line fault; Double line to ground fault; DLGF; Double line-to-ground fault; Line-to-line fault; Bolted fault; Line-to-ground fault; Single line-to-ground fault; Fault (power engineering); Through fault; Incipient fault; Internal fault
общая лексика
сообщение с землей
transient fault
ABNORMAL ELECTRIC CURRENT
Asymmetric fault; Symmetric fault; Transient fault; Persistent fault; Fault current; Electrical faults; Prospective fault current; Earth fault; Restricted earth fault; Fault (electric); Ground Fault; Ground fault; SLGF; Single line to ground fault; Line to line fault; Double line to ground fault; DLGF; Double line-to-ground fault; Line-to-line fault; Bolted fault; Line-to-ground fault; Single line-to-ground fault; Fault (power engineering); Through fault; Incipient fault; Internal fault
нефтегазовая промышленность
неустойчивая неисправность, перемежающаяся неисправность
Definition
page fault
<memory management> In a paged virtual memory system, an
access to a page (block) of memory that is not currently
mapped to physical memory. When a page fault occurs the
operating system either fetches the page in from {secondary
storage} (usually disk) if the access was legitimate or
otherwise reports the access as illegal.
(1995-11-11)
Wikipedia
Fault scarp
A fault scarp is a small step or offset on the ground surface where one side of a fault has moved vertically with respect to the other. It is the topographic expression of faulting attributed to the displacement of the land surface by movement along faults. They are exhibited either by differential movement and subsequent erosion along an old inactive geologic fault (a sort of old rupture), or by a movement on a recent active fault.
