›› 2015, Vol. 36 ›› Issue (1): 1-1.doi: 10.7657/XJPG20150104
• 论文 •
李占东1a,王义军2,胡慧婷1b,王海生3,张海翔1a,李阳4,朱晓萌1a
LI Zhandong1a, WANG Yijun2, HU Huiting1b, WANG Haisheng3, ZHANG Haixiang1a, LI Yang4, ZHU Xiaomeng1a
(1.Northeast Petroleum University, a.Institute of Petroleum Engineering, b.Institute of Earth Sciences, Daqing, Heilongjiang 163318, China; 2. No.1 Oil Production Plant, Daqing Oilfield Company Limited, Daqing, Heilongjiang 163000, China; 3.PetroChina Liaohe Olifiled Company, Panjin, Liaoning 124010, China; 4.Daqing Vocational College, Daqing, Heilongjiang 163255, China)
摘要: 泥页岩层系储集层的性质是决定页岩油藏存在与否的关键因素之一。以松辽盆地北部白垩系青山口组一段泥页岩层系为例,对其烃源岩地球化学特征、矿物含量以及储集空间特征等开展了研究,结果表明:青一段泥页岩层系有机质丰度较高(有机碳含量大都在1%~3%),干酪根类型以Ⅰ型和Ⅱ1型为主,且大部分泥页岩层系正处于生油高峰阶段;脆性矿物含量适中,发育大量不同类型的孔隙,为排烃提供了有效的通道,也为残留在泥页岩层系中的油气提供了充足的储集空间。青一段泥页岩层系整体含油性较好,估算页岩油资源量为78.37×108~97.97×108 t
中图分类号: