Petroleum generation and expulsion characteristics of Lower and Middle Jurassic source rocks on the southern margin of Junggar Basin, northwest China: implications for unconventional gas potential

被引:26
作者
Guo, Jigang [1 ,2 ]
Pang, Xiongqi [1 ,2 ]
Guo, Fengtao [1 ,2 ]
Wang, Xulong [3 ]
Xiang, Caifu [1 ,2 ]
Jiang, Fujie [1 ,2 ]
Wang, Pengwei [1 ,2 ]
Xu, Jing [1 ,2 ]
Hu, Tao [1 ,2 ]
Peng, Weilong [1 ,2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Res Ctr Basin & Reservoir, Beijing 102249, Peoples R China
[3] PetroChina, Xinjiang Oilfield Co, Karamay 834000, Xinjiang, Peoples R China
关键词
SYSTEMS; SHALE; OIL; GEOCHEMISTRY; HAYNESVILLE; MATURATION; BARNETT; MODEL; TEXAS; AREA;
D O I
10.1139/cjes-2013-0200
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Jurassic strata along the southern margin of Junggar Basin are important petroleum system elements for exploration in northwest China. The Lower and Middle Jurassic source rock effectiveness has been questioned as exploration progresses deeper into the basin. These source rocks are very thick and are distributed widely. They contain a high total organic carbon composed predominantly of Type III kerogen, with some Type II kerogen. Our evaluation of source rock petroleum generation characteristics and expulsion history, including one-dimensional basin modeling, indicates that Jurassic source rocks are gas prone at deeper depths. They reached peak oil generation during the Early Cretaceous and began to generate gas in the Late Cretaceous. Gas generation peaked in the Paleogene-Neogene. Source rock shales and coals reached petroleum expulsion thresholds at thermal maturities of 0.8% and 0.75% vitrinite reflectance, respectively, when the petroleum expulsion efficiency was similar to 40%. The petroleum generated and expelled from these source rocks are 3788.75 x 10(8) and 1507.55 x 10(8) t, respectively, with a residual 2281.20 x 10(8) t retained in the source rocks. In these tight reservoirs, a favorable stratigraphic relationship (where tight sandstone reservoirs directly overlie the source rocks) indicates short vertical and horizontal migration distances. This indicates the potential for a large, continuous, tight-sand gas resource in the Lower and Middle Jurassic strata. The in-place natural gas resources in the Jurassic reservoirs are up to 5.68 x 10(12) - 15.14 x 10(12) m(3). Jurassic Badaowan and Xishanyao coals have geological characteristics that are favorable for coal-bed methane resources, which have an in-place resource potential between 3.60 x 10(12) and 11.67 x 10(12) m(3). These Lower and Middle Jurassic strata have good shale gas potential compared with active US shale gas, and the inferred in-place shale gas resources in Junggar Basin are between 20.73 x 10(12) and 113.89 x 10(12) m(3). This rich inferred conventional and unconventional petroleum resource in tight-sand, coal-bed, and shale gas reservoirs makes the deeper Jurassic strata along the southern margin of Junggar Basin a prospective target for future exploration.
引用
收藏
页码:537 / 557
页数:21
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