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鄂尔多斯盆地陇东地区长7段有效烃源岩及生排烃研究
引用本文:郭凯.鄂尔多斯盆地陇东地区长7段有效烃源岩及生排烃研究[J].石油实验地质,2017,39(1):15-23.
作者姓名:郭凯
作者单位:1.中国石油 长城钻探工程有限公司 解释研究中心, 北京 100101
基金项目:国家自然科学基金重点项目“致密砂岩微米—纳米级孔喉网络系统石油充注、运移和聚集机理”(41330319)资助。
摘    要:通过烃源岩地球化学数据分析、测井有机碳计算、生烃潜力法及生排烃史模拟,研究了鄂尔多斯盆地陇东地区长7段有效烃源岩的分布、生排烃史及排烃强度。长7段有机碳含量大于1.0%的暗色泥岩(含油页岩)厚度主要为20~90 m,平均有机碳含量主要介于2%~9%,其有效烃源岩分布以w(TOC)=1.0%和Ro=0.7%为界限,具有大面积广覆式分布的特征;长7段有效烃源岩在侏罗纪末期开始成熟生烃,主要在早白垩世早期(140~130 Ma,Ro≈0.7%)开始排烃,至早白垩世末期(100 Ma)达到生排烃高峰(Ro≈1.0%),最大产油率接近400 mg/g,排油率达308 mg/g,晚白垩世以来的区域性构造抬升使得生烃停止;长7段有效烃源岩排烃强度主要分布于(10~250)×104 t/km2,具有强排烃特征,以长6—长8段致密油为主的延长组油藏主要分布于排烃强度大于20×104 t/km2的地区,油气具有近源短距离富集的特点。 

关 键 词:有效烃源岩    热演化    排烃强度    延长组    三叠系    陇东地区    鄂尔多斯盆地
收稿时间:2016-03-29

Active source rocks of Chang 7 member and hydrocarbon generation and expulsion characteristics in Longdong area,Ordos Basin
Affiliation:1.Geoscience Centre, CNPC Greatwall Drilling Company, Beijing 100101, China2. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China
Abstract:The distribution, hydrocarbon generation and expulsion history and intensity of active source rocks in the Chang 7 member of the Yanchang Formation in the Longdong area of the Ordos Basin were studied based on geoche-mical data, TOC calculation by well logging, hydrocarbon generation potential and expulsion history simulation. Dark mudstone (including oil shale) thickness with an organic carbon content (w(TOC)) more than 1.0% in the Chang 7 member mainly ranges from 20-90 m, and the average w(TOC) is mainly between 2%-9%. Active source rocks of the Chang 7 member have a w(TOC) value over 1.0% and Ro value over 0.7%, and are widely distributed in the Longdong area. They became mature and generated hydrocarbon at the end of Jurassic, expelled hydrocarbon during the early stage of the Early Cretaceous (140-130 Ma,Ro≈0.7%), and reached peak at the end of the Early Cretaceous (100 Ma, Ro≈1.0%). At this time, the oil generation ratio reached 400 mg/g TOC, and the oil expulsion ratio could be 308 mg/g TOC. But oil generation was forced to stop as a result of regional tectonic uplift since the Late Cretaceous. The oil expulsion intensity is mainly (10-250)×104 t/km2, showing the characteristics of strong oil expulsion. Oil reservoirs of the Yanchang Formation dominated with tight oil of the Chang 6-Chang 8 members mainly developed in the area with an oil expulsion intensity over 20×104 t/km2, which indicated that oil accumulation in tight sandstones has characteristics of being near the oil source with a short migration distance. 
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