SIMULATION OF THE SUBSIDENCE AND DEPOSITION OF THE FORELAND BASIN ON THE SOUTHWESTERN MARGIN OF ORDOS
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Abstract:
The subsidence and deposition of the Late Triassic foreland basin on the southwestern margin of Ordos have a close genetic connection with the thrusting of the orogenic belt on both sides of the adjacent Eastern Qilian Mountains. The stratigraphic sequenc
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Liu Shaofeng, Li Sitian, Zhuang Xinguo, Jiao Yangquan, Lu Zongsheng.1996. SIMULATION OF THE SUBSIDENCE AND DEPOSITION OF THE FORELAND BASIN ON THE SOUTHWESTERN MARGIN OF ORDOS[J]. Acta Geologica Sinica,70(1):
