中国准噶尔盆地东部中二叠统卢卡沟源岩的碳氢化合物生成潜力

Deyu Gong , Yihao Miao , Xuan Chen , Hongguang Gou , Tong Lin , Di Li , Runze Yang , Yan Han
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引用次数: 0

摘要

中二叠统卢卡沟地层是准噶尔盆地东部最重要的源岩。先前的研究已经证实,它在吉木萨尔沙格具有极佳的碳氢化合物生成潜力。然而,其在准噶尔盆地东部其他地区的潜力仍不确定。本研究基于总有机碳和热解、有机岩石学、碳氢化合物模拟实验、盆地模拟以及井震耦合解释,系统地比较了吉木萨尔沙格的卢卡沟源岩与准噶尔盆地东部其他地区的碳氢化合物生成潜力。研究讨论了优质源岩的沉积环境,并描绘了实用源岩套件的分布。准噶尔盆地东部的卢草沟源岩属于易生油岩,以I-II型角质岩为主,一般被划分为良好至极佳的源岩。目前,卢草沟源岩进入主生油窗口的面积约为 11×103 平方公里。除隆起区外,准噶尔盆地东部的卢草沟源岩先后于侏罗纪进入油气生成临界期和白垩纪进入主生油窗口期。吉木萨尔沙格和准噶尔盆地东部其他地区的卢卡沟源岩具有相似的生物标志物指纹,其特征是Pr/Ph、Pr/n-C17、Tm/C30 hopane、C19/C20三环萜烯和C24四环萜烯/C26三环萜烯的比率相对较低,而β-胡萝卜素含量、伽马塞烷指数和Ts/Tm比率较高。这些特征反映了在强还原性咸水湖环境中的沉积情况,亲本来源以藻类和细菌等低等生物为主。一般来说,准噶尔盆地东部卢卡沟源岩的产油强度超过 3 × 106 吨/平方公里。在博格达山前带、吉木萨尔下陷、东道海子下陷、五彩湾下陷和沙张断裂带上发育了多个生油强度大于 5×106 t/km2 的生油中心,总面积约 12500 平方公里。卢草沟源岩的这些特征为形成大、中型油田提供了有利条件。该成果进一步巩固了准噶尔盆地东部的油气资源,为今后勘探油气田提供了宝贵的参考依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrocarbon-generating potential of the Middle Permian Lucaogou source rock in the eastern Junggar Basin, China

The Middle Permian Lucaogou Formation is the most significant source rock in the eastern Junggar Basin. Previous studies have confirmed its excellent hydrocarbon-generating potential in the Jimsar Sag. However, its potential in other areas of the eastern Junggar Basin remains uncertain. Based on total organic carbon and pyrolysis, organic petrology, hydrocarbon simulation experiments, basin simulation, and combined well-seismic coupling interpretation, this study systematically compares the hydrocarbon-generating potential of the Lucaogou source rock in the Jimsar Sag with other areas of the eastern Junggar Basin. It discusses the sedimentary environment of high-quality source rocks and depicts the distribution of practical source kitchens. The Lucaogou source rocks in the eastern Junggar Basin are oil-prone, dominated by type I–II kerogen, and generally classified as good to excellent source rocks. Nowadays, the area of the Lucaogou source rocks that have entered the main oil-generating window is approximately 11 × 103 km2. Except for the bulge area, the Lucaogou source rocks in the eastern Junggar Basin successively entered the hydrocarbon-generating threshold during the Jurassic and the main oil-generating window in the Cretaceous. The Lucaogou source rocks in the Jimsar Sag and other parts of the eastern Junggar Basin share similar biomarker fingerprints, characterized by relatively low ratios of Pr/Ph, Pr/n-C17, Tm/C30 hopane, C19/C20 tricyclic terpene, and C24 tetracyclic terpene/C26 tricyclic terpene, and high β-carotene content, gammacerane index, and Ts/Tm ratios. These characteristics reflect deposition in a strongly reducing brackish lacustrine environment with parental sources dominated by lower organisms such as algae and bacteria. Generally, the Lucaogou source rocks in the eastern Junggar Basin have an oil-generating intensity of more than 3 × 106 t/km2. Several oil-generating centers with an intensity of more than 5 × 106 t/km2 have developed in the front of the Bogda Mountain, Jimsar Sag, Dongdaohaizi Sag, Wucaiwan Sag, and Shazhang Fault Zone, covering a total area of approximately 12,500 km2. These characteristics of the Lucaogou source rocks promise favorable potential for forming large and medium oil fields. The results further consolidated the oil and gas resources in the eastern Junggar Basin and provided valuable references for exploring future oil and gas fields.

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