Petroleum Exploration and Development-Forthcoming Articles Forthcoming Articles http://www.cpedm.com EN-US http://www.cpedm.com/EN/current.shtml http://www.cpedm.com 5 <![CDATA[Characteristics and discovery significance of the Upper Triassic-Lower Jurassic marine shale oil in Qiangtang Basin, NW China]]> 1 and II2, with the average TOC of 8.34%, the average content of chloroform bitumen 'A' of 0.66%, the average residual hydrocarbon generation potential (S1+S2) of 29.93 mg/g, and the Ro value of 0.9%-1.3%, meeting the standard of high-quality source rock. The organic-rich shale of the Bagong Formation contains mixed organic matters, with the TOC of 0.65%-3.10% and the Ro value of 1.17%-1.59%, meeting the standard of moderate source rock. Fourth, four shallow wells (depth of 50-250 m) showed oil flower respectively in the organic shales at 50-90 m in the lower part of the Bagong Formation and 30-75 m in the middle part of the Quse Formation. The crude oil contains a high content of saturated hydrocarbon. Analysis and testing of outcrop and shallow well samples confirm the presence of marine shale oil in the Bagong Formation and the Quse Formation. Good shale oil intervals in the Bagong Formation are observed in Layers 18-20 in the lower part of the section, where the shales with (S0+S1)˃1 mg/g are 206.7 m thick, with the maximum and average (S0+S1) of 1.92 mg/g and 1.81 mg/g, respectively. Good shale oil intervals in the Quse Formation are found in Layers 4-8 in the lower part of the section, where the shales with (S0+S1)˃1 mg/g are 58.8 m thick, with the maximum and average (S0+S1) of 6.46 mg/g and 2.23 mg/g, respectively.]]> <![CDATA[Key technologies and practice for gas field storage facility conversion of complex geological conditions in China]]> <![CDATA[Multistage interwell tracing for step-by-step profile control of water channeling and flooding of ultra-low permeability reservoirs]]> <![CDATA[Water and gas distribution and its controlling factors for large scale tight sand gas fields: A case study of western Sulige gas field, Ordos Basin, NW China]]> <![CDATA[Type, characteristics and effect of natural fluid pressure fractures in shale: A case study of the Paleogene strata in Eastern China]]>