Übersetzung und Analyse von Wörtern durch künstliche Intelligenz
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FAULTING - Übersetzung nach arabisch
![Sault Ste. Marie]], Northern Ontario, Canada](https://commons.wikimedia.org/wiki/Special:FilePath/CREIGHTON-fault-sudbury-basin-science-north.jpg?width=200 "Sault Ste. Marie]], Northern Ontario, Canada")
![Normal fault in [[La Herradura Formation]], [[Morro Solar]], Peru. The light layer of rock shows the displacement. A second normal fault is at the right.](https://commons.wikimedia.org/wiki/Special:FilePath/Falla normal Morro Solar Peru.jpg?width=200 "Normal fault in [[La Herradura Formation]], [[Morro Solar]], Peru. The light layer of rock shows the displacement. A second normal fault is at the right.")
![Salmon-colored [[fault gouge]] and associated fault separates two different rock types on the left (dark gray) and right (light gray). From the [[Gobi]] of [[Mongolia]].](https://commons.wikimedia.org/wiki/Special:FilePath/FaultGouge.JPG?width=200 "Salmon-colored [[fault gouge]] and associated fault separates two different rock types on the left (dark gray) and right (light gray). From the [[Gobi]] of [[Mongolia]].")
![A fault in [[Morocco]]. The fault plane is the steeply leftward-dipping line in the centre of the photo, which is the plane along which the rock layers to the left have slipped downwards, relative to the layers to the right of the fault.](https://commons.wikimedia.org/wiki/Special:FilePath/Fault in Seppap Gorge Morocco.jpg?width=200 "A fault in [[Morocco]]. The fault plane is the steeply leftward-dipping line in the centre of the photo, which is the plane along which the rock layers to the left have slipped downwards, relative to the layers to the right of the fault.")
.jpg?width=200 "Normal fault and drag folds (eastern flanks of the Bighorn Mountains, Wyoming, USA)")
ألاسم
اِنْشِقاق ; اِنْفِلاق ; بَتّ ; بَتْر ; بَضْع ; تَشَقُّق ; تَصَدُّع ; تَفْلِيق ; جَزْم ; شَرْم ; شَقّ ; شِقّ ; صَدْع ; صِير ; فَتْق ; فَطْر ; فَلْج ; فَلْع ; فَلْق
الفعل
عابَ ; عَيَّبَ ; لَسَنَ ; لَمَزَ
Definition
Wikipedia
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep.
A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault.
A fault zone is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the distinction, as the rock between the faults is converted to fault-bound lenses of rock and then progressively crushed.
