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Petroleum Geochemistry of the Loperot-1 Well in Lokichar Basin, Kenya

机译:肯尼亚洛克盆地Lokichar-1的石油地球化学

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The work reports an in-depth review of bulk and molecular geochemical data to determine the organic richness, kerogen type and thermal maturity of the Lokhone and the stratigraphically deeper Loperot shales of the Lokichar basin encountered in the Loperot-1 well. Oil-source rock correlation was also done to determine the source rocks’ likelihood as the source of oil samples obtained from the well. A combination of literature and geochemical data analyses show that both shales have good to excellent potential in terms of organic and hydrogen richness to act as conventional petroleum source rocks. The Lokhone shales have TOC values of 1.2% to 17.0% (average 5.16%) and are predominantly type I/II organic matter with HI values in the range of 116.3 - 897.2 mg/g TOC. The Lokhone source rocks were deposited in a lacustrine depositional environment in episodically oxic-dysoxic bottom waters with periodic anoxic conditions and have T_(max) values in addition to biomarker signatures typical of organic matter in the mid-mature to mature stage with respect to hydrocarbon generation and immature for gas generation with Ro values of 0.51 - 0.64%. The Loperot shales were shown to be possibly highly mature type II/III source rocks with TOC values of 0.98% - 3.18% (average 2.4%), HI of 87 - 115 mg/g TOC and Ro of 1.16 - 1.33%. The Lokhone shale correlate well with the Loperot-1 well oils and hence is proposed as the principal source rock for the oils in the Lokichar basin. Although both source rocks have good organic richness to act as shale gas plays, they are insufficiently mature to act as shale gas targets but this does not preclude their potential deeper in the basin where sufficient gas window maturities might have been attained. The Lokhone shales provide a prospective shale oil play if the reservoir suitability to hydraulic fracturing can be defined. A basin wide study of the source rocks thickness, potential, maturation and expulsion histories in the Lokichar basin is recommended to better understand the present- day distribution of petroleum in the basin.
机译:该工作报告了对批量和分子地球化学数据的深入审查,以确定Lokhone的有机丰富,Kerogen型和热成熟度,并良好地遇到的Lokichar盆地的地层较深的Loperot Shales。还进行了油源岩体相关性以确定源岩石的可能性,因为从井中获得的油样品源。文献和地球化学数据分析的组合表明,两只神均在有机和氢气方面具有良好的潜力,以充当常规石油源岩石。 Lokhone Shales的TOC值为1.2%至17.0%(平均5.16%),主要是I / II有机质型,HI值在116.3-897.2mg / g TOC的范围内。 Lokhone源岩在具有周期性缺氧条件下的整形氧 - 堤底部水处沉积在展开症状环境中,除了在成熟中典型的有机物质的生物标志物签名,还具有相对于烃的成熟阶段的生物标志物签名之外的T_(最大值)值对汽油产生的产生和不成熟,RO值为0.51-0.64%。显示叶片罗贝雷斯可能是高度成熟的II / III源岩,TOC值0.98% - 3.18%(平均2.4%),HI为87-115mg / g TOC,RO为1.16-1.33%。 Lokhone Shale与Loperot-1孔油相关,因此建议作为Lokichar盆地油的主要源岩。虽然两个来源岩石都有良好的有机丰富性,但作为页岩气相的起法,它们不够成熟,以充当页岩气目标,但这并不排除其在盆地中的潜力更深,其中可能已经实现了足够的气体窗口的井地性质。如果可以定义液压压裂的水库适用性,Lokhone Shales提供了一个未来的页岩油。建议在Lokichar盆地的源岩厚度,潜在,成熟和排出历史的源岩厚度,更好地了解盆地中石油的本日分布。

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