WebThe Jiuxi (Western Jiuquan) Basin, located in the west of the Hexi Corridor, NW China, is a foreland basin which has been active since the Early Jurassic. It was formed as a consequence of the progressive northwards migration of the North Qilian thrusts in response to sinistral shearing along the 2,000‐km long Aerjin (Altun) Fault. WebMay 4, 2009 · The remains of the load system responsible for flexure of the South China foreland can be seen in the Songpan-Ganzi Fold Belt and Longmen Shan Thrust Belt. Early in its history the Longmen Shan Foreland Basin extended well beyond its present northwestern boundary along the trace of the Pengguan Fault, to at least the …
Pet.Sci.(2008)5:83-86 DOI 10.1007/s12182-008-0014-4 …
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WebDec 18, 2007 · The Jiuxi (Western Jiuquan) Basin, located in the west of the Hexi Corridor, NW China, is a foreland basin which has been active since the Early Jurassic. It was … WebMay 15, 2024 · A northwest-tapering retro-arc foreland system is traced in northwest South China. • Tectonic processes in the arc-retroarc system were linked and governed mass transfer. • Intraplate processes were related to subducting geodynamics of the Paleo-Pacific plate. Keywords seismic reflection retro-arc foreland decollement South China … WebDepression basins were mainly developed during Mesozoic era, such as the Songliao Basin (K) in eastern China, the Ordos Basin (K) in central China. Foreland basins were dominantly formed during Mesozoic era and late Paleozoic era, such as the western area of the Sichuan Basin (T). incheon or gimpo airport