Late Quaternary tectonic activity and crustal shortening rate of the Bogda mountain area, eastern Tian Shan, China
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文摘

The crustal shortening rate of the Fukang fault is 0.90 ± 0.20 mm/yr.

The geomorphic surfaces in the Bogda northern piedmont area are divided.

The Bogda mountain is a thick–skinned nappe whose deformation characteristic is dominated by vertical uplift.

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