【摘 要】
：
1 Introduction There is a set of organic rich shale at E22S4sub-member in damnintun sag.The organic material is typically type I.In recent years,breakthrough wa
【机 构】
：
China University of Petroleum(East China),Liaohe Oil Field Company of CNPC,
【出 处】
：
Acta Geologica Sinica(English Edition)
论文部分内容阅读
1 Introduction There is a set of organic rich shale at E22S4sub-member in damnintun sag.The organic material is typically type I.In recent years,breakthrough was obtained in shale oil exploration.The wettability of organic and inorganic pore is different.As a result,the mobility of oil in organic and inorganic pore is different.So it’s necessary to distinguish
1 Introduction There is a set of organic rich shale at E22S4sub-member in damnintun sag. The organic material is typically type I. In recent years, breakthrough was obtained in shale oil exploration. The wettability of organic and inorganic pore is different. As a result, the mobility of oil in organic and inorganic pore is different. So it’s necessary to distinguish
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