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Quantitative modelling of hydrocarbon expulsion and quality grading of tight oil lacustrine source rocks: Case study of Qingshankou 1 member, central depression, Southern Songliao Basin, China

机译:岩土源岩的碳氢化合物驱逐和质量分级的定量建模 - 南志库1成员案例研究,中部萧条南部南部松辽盆地

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The quality of source rocks plays an important role in the distribution of tight and conventional oil and gas resources. Despite voluminous studies on source rock hydrocarbon generation, expulsion and overpressure, a quality grading system based on hydrocarbon expulsion capacity is yet to be explored. Such a grading system is expected to be instrumental for tight oil and gas exploration and sweet spot prediction. This study tackles the problem by examining Late Cretaceous, lacustrine source rocks of the Qingshankou 1 Member in the southern Songliao Basin, China. By evaluating generated and residual hydrocarbon amounts of the source rock, the extent of hydrocarbon expulsion is modelled through a mass balance method. The overpressure is estimated using Petromod software. Through correlation between the hydrocarbon expulsion and source rock evaluation parameters [total organic carbon (TOC), kerogen type, vitrinite reflectance (R-0) and overpressure], three classes of high-quality, effective and ineffective source rocks are established. High-quality class contains TOC >2%, type-I kerogen, R-0 >1.0%, overpressure >7Mpa, sharp increase of hydrocarbon expulsion along with increasing TOC and overpressure, and high expulsion value at R-o >1%. Source rocks with TOC and R-o <0.8%, type-II2 & III kerogen, overpressure <3Mpa, and low hydrocarbon expulsion volume are considered ineffective. Rocks with parameters between the two are considered effective. The high-quality class shows a strong empirical control on the distribution of tight oil in the Songliao Basin. This is followed by the effective source rock class. The ineffective class has no measurable contribution to the tight oil reserves. Because the hydrocarbon expulsion efficiency of source rocks is controlled by many factors, the lower limits of the evaluation parameters in different basins may vary. However, the classification method of tight source rocks proposed in this paper should be widely applicable. (C) 2017 Elsevier Ltd. All rights reserved.
机译:源极岩的质量在紧张和常规石油和天然气资源的分布中起着重要作用。尽管对源岩石烃产生的巨大研究,驱逐和过压,但尚未探索基于碳氢化合物驱逐产能的质量分级系统。预计这种分级系统将是纯粹的石油和天然气勘探和甜点预测的乐器。本研究通过检查中国松辽盆地南部青春沟1成员的后期白垩纪,湖泊源岩来解决问题。通过评估产生的烃源岩的生成和残留的烃量,通过质量平衡法模拟烃排出的程度。使用PetroMod软件估算过压。通过碳氢化合物驱逐和源岩评估参数之间的相关性[总有机碳(TOC),Kerogen型,Vitriinite反射(R-0)和过压],建立了三类高质量,有效和无效的源岩。高质量的阶级含有TOC> 2%,I型Kerogen,R-0> 1.0%,过度压力> 7MPa,碳氢化合物驱逐的急剧增加以及增加的TOC和过压,以及R-O> 1%的高排出值。具有TOC和R-O <0.8%的源岩,II2型和III Kerogen,超压<3MPa和低碳氢化合物驱逐体积被认为是无效的。两者之间参数的岩石被认为是有效的。高质量的阶级对松辽盆地紧密油分布的强大实证控制。这是有效的源摇滚类。无效的课程对紧密石油储备没有可衡量的贡献。因为源岩的烃排出效率受到许多因素的控制,所以不同盆地评估参数的下限可能变化。然而,本文提出的紧源岩的分类方法应广泛适用。 (c)2017 Elsevier Ltd.保留所有权利。

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