thrust fault
Quick Summary
A thrust fault is a type of geological fault where the angle between the horizontal and the fault plane is small. It is also known as an overthrust fault.1
In geology, a fault is a fracture in the Earth's crust where rocks on opposite sides move relative to each other due to compressional or tensional forces. Thrust faults specifically result from horizontal compressional forces that shorten the Earth's crust. In this type of fault, the hanging wall (the block above the fault plane) moves up and over the footwall (the block below the fault plane). Thrust faults are a type of reverse fault with a dip less than 45 degrees and are commonly found in intensely deformed mountain ranges.2
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faultReverse dip-slip faults result from horizontal compressional forces caused by a shortening, or contraction, of Earth’s crust. The hanging wall moves up and over the footwall. Thrust faults are reverse faults that dip less than 45°. Thrust faults with a very low angle of dip…
Read MoreReverse dip-slip faults result from horizontal compressional forces caused by a shortening, or contraction, of Earth’s crust. The hanging wall moves up and over the footwall. Thrust faults are reverse faults that dip less than 45°. Thrust faults with a very low angle of dip…
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metamorphic rockStructural features…the Main Central Thrust, a thrust fault that runs for hundreds of kilometres from east to west and was responsible for the transportation of rocks belonging to the Eurasian Plate southward over those of the Indian Plate. Along much of the length of this fault, the metamorphic rocks in the…
Read More…the Main Central Thrust, a thrust fault that runs for hundreds of kilometres from east to west and was responsible for the transportation of rocks belonging to the Eurasian Plate southward over those of the Indian Plate. Along much of the length of this fault, the metamorphic rocks in the…
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