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The Shunnan (SN) area, located in the center of the Tarim basin, NW China, is a gas field discovered in 2013, where the gas is hosted from deeply buried Ordovician carbonate reservoirs with burial depth>6000m and temperature>190°C. The most important reservoir rocks in the SN area are silicified limestones, which are characterized by multiple generations/types of authigenic quartz (Qz1–Qz2)...
Coarse clastic rocks, developed widely at foredeep adjacent to orogene, were usually regarded as the mark of renewed thrusting action. However a good example from the Lower Cretaceous in Kuqa foreland sub-basin illustrated that the coarse clastic rocks developed not only in initial thrusting stage but in early quiescence stage. The Kuqa foreland sub-basin, adjacent to the south Tianshan Orogene, lies...
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