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- W2355164098 abstract "The rotations is produced not only by the large movement of the main strike-slip fault,but also by the horizontal movement of the secondary faults within the main fault or in the adjacent area.Although some dynamic models have been proposed to illustrate the relationship between vertical axis rotations and fault slips,it is very difficult to find a simple model to explain the mechanism of the rotations and strike-slip fault systems because of the difference of the deformation environment and boundary conditions in different strike-slip fault systems.In many strike-slip tectonic settings,rotations of faults and blocks have been inferred from both laboratory modeling and field geological surveys.Studies show that tectonic rotations related strike-slip faults are very distinct in the areas such as the western coast near the San Andreas fault,the Lake Mead fault in the Basin and Range Province in the United States,the Ailaoshan-Red River fault in Southeast China,the Alpine fault in New Zealand and the Northern Anatolian fault in Turkey.The methods of paleomagnetism,magnetic fabric,tectonic analysis,high-accuracy GPS monitoring and tectonic modeling can be used to identify these rotations,but the combination of the methods are very important to get a reliable result.Much attention should be paid to the tectonic regime and geography changes resulted from tectonic and block rotations during the study of the strike-slip faults,especially the large-scale strike-slip fault systems." @default.
- W2355164098 created "2016-06-24" @default.
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- W2355164098 date "2006-01-01" @default.
- W2355164098 modified "2023-09-27" @default.
- W2355164098 title "A Review on Tectonic Rotations Related to Large Strike-Slip Faults" @default.
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