阿尔金山南缘侏罗系页岩气生烃及储集条件
Shale-gas hydrocarbon generation and accumulation conditions of the Jurassic strata in southern Altun Mountains
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摘要: 柴达木盆地阿尔金山南缘侏罗系发育, 具备油气生成的条件, 但尚未开展页岩气调查评价。通过野外地质测量和样品采集分析, 调查了侏罗纪泥页岩发育的厚度、沉积环境, 分析了页岩地球化学、储层物性等页岩气地质条件。研究表明, 侏罗纪泥页岩累计厚度介于158~250m之间, 单层最大厚度89m;沉积环境以深湖-半深湖为主; 有机碳含量介于0.15%~7.96%之间, 平均2.05%;镜质体反射率介于1.02%~2.50%之间, 平均1.41%;有机质类型以Ⅱ1和Ⅱ2型为主; 泥页岩微裂缝及微孔隙发育, 脆性矿物平均含量大于43%。综合分析认为, 阿尔金山南缘侏罗系泥页岩具有较好的页岩气生烃和储集条件, 可作为页岩气勘查开发的有利层系Abstract: Jurassic strata, which are well developed in southern Altun Mountains, have good oil and gas generation conditions; never-theless, no investigation and evaluation for shale gas have been carried out in this region. Based on field geological survey and sample test, the authors investigated the thickness and sedimentary environment of Jurassic shale and analyzed the geochemical and reservoir property conditions of shale gas. The results show that the total thickness of Jurassic mudstone is 158~250m with the largest single thickness up to 89 m. Sedimentary environment is deep lake and semi-deep lake depositional facies. Organic carbon content is 0.15%~7.96% with an average of 2.05%. Vitrinite reflectance is 1.02%~2.50% with an average of 1.41%. Kerogen types are mainly typeⅡ1 and typeⅡ2. The shale layers also contain high content of brittle minerals(>43%), with effective reservoir space well developed in the shales. The comprehensive analysis indicates that the Jurassic shale in southern Altun Mountains has basic geological conditions for shale-gas generation and accumulation.