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- W2350200062 abstract "Surface observations along the nearly N-S-trending Western Wenquan basin marginal fault in the interior of the Tanggula Mountains show that this fault underwent multi-stage activities during the late Quaternary. Along the fault we may recognize at least eight fault scarps or steep fault slopes whose heights are 0.33-0.62 m, 4.3-5.2 m, 6.8-8.3 m, 10-11.8 m, ～16 m, 20-28 m, 45-50 m and 65-80 m respectively, as well as river terraces, diluvial fans and spring sinter platforms that may largely correspond with these fault scarps. Analysis of the relative ages of geologic-geomorphologic bodies and U-series and ESR dating of calcareous coatings of pebbles and calcareous cements in spring sinters and stream sediments indicate that the fault scarps with heights of 45-50 m, 20-28 m, ～16 m, 10-11.8 m, 6.8-8.3 m and 4.3-5.2 m formed at ～127 ka BP, 54 ka BP, 25 ka BP, 18 ka BP, 11 ka BP and since 4 ka BP. The intensities of faulting were different in different periods. The average rates of vertical movements of the fault during ～127-25 ka BP, 25-4 ka BP and 4-1.1 ka BP were 0.3-0.23 mm/a, 0.8-0.36 mm/a and 1.65 mm/a respectively." @default.
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- W2350200062 date "2005-01-01" @default.
- W2350200062 modified "2023-09-27" @default.
- W2350200062 title "Geomorphologic indicators and rates of late Quaternary normal faulting at the west side of the Wenquan graben, central Qinghai-Tibet Plateau," @default.
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