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- W2384310707 abstract "Two second-order structural units are divided in Qimugen-Sangzhuhe area, i.e., Tiekelike fault uplift and southwestern Tarim depression. Four third-order structural units are further divided in southwestern Tarim depression, including Qimugen uplift, Keziletag depression, Yecheng-Hotan depression and Tiekelike northern margin slope. The thrust-nappe structures comprise the major structural style. Two large ones formed during the end of Hercynian stage and end of Himalayan stage. Root zone, median zone, frontal zone and outer zone are further differentiated along the thrust direction of nappe. Associated with thrust-nappe structures are, from south to north, Tanmu-Qiketashi-Pusha-Yuliqun- Sangzhu steep anticline zone, Tongyouluke-Yiliyasi-Kaokuya-Artashi-Qipan-Kekeya intermediate anticline zone and Guman-Heshitake low anticline zone. The boundary fault No.20 separating Keziletage depression and Yecheng-Hotan depression is a regional-scale one initiated from the Paleozoic, which controls sedimentation on both sides. The study area underwent 6 stages of development, from basement, rift-depression basin at margins of craton, intra-craton compressional basin, intra-craton depression basin, foreland basin to unified inland basin." @default.
- W2384310707 created "2016-06-24" @default.
- W2384310707 creator A5039930405 @default.
- W2384310707 date "2002-01-01" @default.
- W2384310707 modified "2023-09-25" @default.
- W2384310707 title "STRUCTURES OF QIMUGEN-SANGZHUHE AREA" @default.
- W2384310707 hasPublicationYear "2002" @default.
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