How To Use Strike-slip fault In A Sentence
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It extends parallel to Xianshuihe fault, which is a major active sinistral strike-slip fault in eastern Tibet Plateau.
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It is commonly assumed that the Stanovoy sinistral shear zone and the Sakhalin-Hokkaido dextral shear zone in NE Asia are two conjugate strike-slip faults related to the India-Eurasia collision.
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Strike-slip fault and overthrust and syn and anticline…
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In fact, Aleksandrowski et al proposed that the complex was originally contiguous with the Northern Phyllite Zone in Germany and that dextral strike-slip fault movement translated this region southeastward to its present position.
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It is concluded that this strike-slip fault is in tensoshear property and should be lagging products associated with reverse fault of NE trend.
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Although data on vertical displacement on the Klima fault zone are limited, the horizontal component is clearly much larger, and the Klima fault zone represents a sinistral strike-slip fault.
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This paper tentatively identifies two lineaments and a fault that may relate to sinistral strike-slip faulting in the pre-Paradox Formation basement beneath Upheaval Dome.
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Deposition of the unconformably overlying Red Bay Group was terminated in latest Lochkovian times by renewed sinistral strike-slip faulting.
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Berndt infers a pull-apart basin as the reason for this local depression, because of the location between two major strike-slip faults.
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The main fracture of the western margin fault zone of the South China Sea is originated from the Mesozoic basement fault, continuously developed into dextral strike-slip fault zone in Cenozoic.
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Both strike-slip faults and thrusts, commonly at high angles, are present.
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Much of the Apennine chain has been dissected by normal and strike-slip faults that locally post-date thrust structures.
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In conclusion, the geological characteristics of the South China Sea cannot be explained by a pull-apart model involving a releasing bend of a sinistral strike-slip fault.
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They show that the bounding faults of the "graben" cut the Chumstick Formation and that the southwestern bounding fault really is a composed of northwesterly trending reverse faults and younger northerly strike-slip faults, both of which cut northwesterly striking folds in the Chumstick Formation.
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Shortening is manifested by the development of folds and thrust faults; the horizontal slip is accommodated by strike-slip faults.
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These subterranean muds are being uplifted into steeply dipping, anticlinal structures cored by strike-slip faulting.
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It indicated that normal faulting processes induced from the shear of dextral strike-slip faults are active in the historically subsiding Tainan basin.
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The Murzinka-Adui Metamorphic Complex to the SE of the Salda Complex is separated from the latter by the Petrokamensk Arc and the Sisert dextral strike-slip fault.
