supported by the SINOPEC Forward Looking Project of China (No. YPH08114)
A great amount of quartz was found filling vugs of the dolomite strata of Upper Cambrian-Lower Ordovician in Keping (柯坪) outcrop area of Tarim basin, China, which is widely distributed with obvious impact on dolom...
supported by the SINOPEC Forward Looking Project of China(No.YPH08114);Petrochemical Joint Fund (No.40839910);the Central University of Special Funds of China(No.CUGL120253);the Young Teacher Founding Project of China University of Geosciences(No. CUGQNL0826)
The Carboniferous Karashayi (卡拉沙依) Formation of Tarim basin formed in the epicontinental sea shelf environment where the evolution of basins is pediocratic. As an important reservoir-forming combination, the Car...
supported by the SINOPEC Forward Looking Project of China (No. YPH08114)
The reef-shoal depositional system of the Ordovician carbonate platform margin is well exposed in the Yijianfang (一间房) outcrop of the Bachn (巴楚) uplift region, which offers an advantageous condition to study ...
supported by the SINOPEC Forward Looking Project of China (No. YPH08114)
The oolitic shoals of the Triassic carbonate platform margin in the Yudongzi (鱼洞子) outcrop of Erlangmiao (二郎庙) area in the northwestern Sichuan (四川) basin present a scarce opportunity to quantitatively d...
supported by the SINOPEC Forward Looking Project of China (No. YPH08114);Petrochemical Joint Fund(No. 40839910);the Young Teacher Funding Project of China University of Geosciences (No. CUGQNL0826)
The Cenozoic reef-banks reservoir in Qiongdongnan (琼东南) basin is one of the most profitable targets worthy of prospecting in the deep water area of the northwestern South China Sea. In this study, the characteris...