Hydrocarbon-generating potential of the Middle Permian Lucaogou source rocks in the Gucheng Sag, Junggar Basin, China

Deyu Gong , Yan Han , Tanguang Fan , Xinning Li , Chuanmin Zhou , Shoqing Wang , Ruiju Wang , Wei'an Wu , Yihao Miao
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Abstract

A billion-ton mega shale oil field has been discovered in the Jimsar Sag, located in the Eastern Uplift of Junggar Basin, which reveals the good hydrocarbon-generating potential of the source rocks in the Middle Permian Lucaogou Formation. This paper systematically evaluates the hydrocarbon-generating potential and formation environment of the Lucaogou source rocks in the Gucheng Sag, which is adjacent to the Jimsar Sag, and draws the distribution range of the source kitchen, and compares them with those of the Lucaogou source rocks in the Jimsar Sag. The results show that the kerogen type of Lucaogou source rocks in the Gucheng Sag is mainly of type II/III–III, dominated by good–excellent source rocks, and the type and abundance are slightly inferior to those in the Jimusar Sag. In the Middle and Late Jurassic, the Lucaogou source rocks in the Gucheng Sag entered the hydrocarbon-generating threshold, and now, the area entering the main oil-generating window reaches 212 km2. Although both of them are lacustrine deposits, the Lucaogou source rocks in the Gucheng Sag have slightly higher Pr/Ph, Ts/(Ts + Tm), C19/C21 tricyclic terpane, C24 tetracyclic terpane/C26 tricyclic terpane ratios, and somewhat lower C28 regular sterane content than the Jimsar Sag, suggesting that Lucaogou source rocks were deposited in an oxidizing–reducing transitional environment of a specific salinity in the Gucheng Sag. There was a certain amount of terrestrial higher plant input in addition to the contribution of algal and microbial biota in the Lucaogou source rocks in the Gucheng Sag. The Lucaogou source rocks have developed four centers with a thickness greater than 160 m in the Gucheng Sag, covering a total area of about 420 km2. In the southern part of the sag, three hydrocarbon-generating centers with an oil-generating intensity greater than 2000 × 103 t/km2 have developed, covering a total area of 130 km2. The research results further strengthen the resource base of the Middle Permian petroleum system in the Junggar Basin and lay the foundation for the next step of petroleum exploration in the Gucheng Sag.
准噶尔盆地古城凹陷中二叠统芦草沟烃源岩生烃潜力
准噶尔盆地东隆起吉木萨尔凹陷发现十亿吨大型页岩油田,揭示了中二叠统芦草沟组烃源岩具有良好的生烃潜力。本文系统评价了与吉木萨尔凹陷相邻的古城凹陷芦草沟烃源岩的生烃潜力和形成环境,绘制了烃源灶分布范围,并与吉木萨尔凹陷芦草沟烃源岩进行了对比。结果表明:古城凹陷芦草沟烃源岩干酪根类型以ⅱ/ⅲ~ⅲ型为主,以优良型烃源岩为主,类型和丰度略低于吉木萨尔凹陷。中晚侏罗世谷城凹陷芦草沟烃源岩进入生烃阈值,目前进入主生油窗口面积达212 km2。古城凹陷芦草沟烃源岩的Pr/Ph、Ts/(Ts + Tm)、C19/C21三环萜烷、C24四环萜烷/C26三环萜烷比值略高于吉木萨凹陷,C28规则甾烷含量略低于吉木萨凹陷,表明芦草沟烃源岩形成于古城凹陷特定盐度的氧化还原过渡环境。谷城凹陷芦草沟烃源岩除了有藻类和微生物的贡献外,还存在一定的陆生高等植物的输入。芦草沟烃源岩在谷城凹陷发育4个厚度大于160 m的烃源岩中心,总面积约420 km2。凹陷南部发育3个生油强度大于2000 × 103 t/km2的生烃中心,总面积达130 km2。研究成果进一步夯实了准噶尔盆地中二叠统含油气系统的资源基础,为古城凹陷下一步油气勘探奠定了基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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