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Deep-Lacustrine Shale Heterogeneity and Its Impact on Hydrocarbon Generation, Expulsion, and Retention: A Case Study from the Upper Triassic Yanchang Formation, Ordos Basin, China

机译:深层湖泊物流异质性及其对烃生成,驱逐和保留的影响:以鄂尔多斯盆地,鄂尔多斯盆地地区延长三叠系延长地区的案例研究

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The Chang-7 shale of the Upper Triassic Yanchang Formation was deposited in a deep-lacustrine environment in the southwest part of the Ordos Basin. It is characterized by a strong lithological heterogeneity, consisting primarily of pure shale and sandy laminated shale. This study explored the impact of sandy laminae in the thick pure shale on hydrocarbon generation, retention, and expulsion, which were rarely considered in previous studies. Based on core observation, thin section, and geochemical analysis, the hydrocarbon generation, retention, and expulsion characteristics were obtained for both pure shale and sandy laminated shale. In general, the Chang-7 shale stays at low mature to mature thermal evolution stage and has good hydrocarbon generation potential. It contains mainly Type II kerogen with an average total organic carbon (TOC) of 2.9% and average (S-1+S-2) of 8.2mg/g. Compared with sandy laminated shale, pure shale contains more retained liquid hydrocarbon and has a higher amount of asphaltene and nitrogen-sulfur-oxygen (NSO) polarized components, indicating a relatively weak hydrocarbon expulsion process. The middle part of a thick pure shale retains more liquid hydrocarbon and has higher percentages of asphaltene and NSO polarized components than that of the top and basal part of the shale where sandy laminae occur. The difference in hydrocarbon retention capacity is interpreted to have been primarily caused by the comparatively higher reservoir quality of the sandy laminated shale, having higher amount of brittle minerals and larger pores than the pure shale. Polymer dissolution and nanopore adsorption are also key factors in hydrocarbon retention and component partition. Based on this study, we suggest that sandy laminated shale, which receives most of the hydrocarbon from adjacent pure shale, should be the current favorable shale oil exploration targets. Even though pure shale contains high hydrocarbon potential, its development is still pending improved technologies, which could solve the challenges caused by complicated geological conditions.
机译:鄂尔多斯盆地西南部的深层湖泊环境中的Chang-7页岩沉积在深章外的环境中。它的特点是强烈的岩性异质性,主要由纯页岩和砂层层状页岩组成。本研究探讨了砂质薄层在粗纯页岩上的碳氢化合物发电,保留和排出的影响,这很少在先前的研究中考虑。基于核心观察,薄剖面和地球化学分析,为纯页岩和砂层叠层页岩获得碳氢化合物产生,保留和排出特性。通常,Chang-7页岩在成熟的低成熟度到成熟的热演化阶段,具有良好的碳氢化合物产生电位。它主要含有II型Kerogen,平均总有机碳(TOC)为2.9%,平均(S-1 + S-2)为8.2mg / g。与桑迪层压页岩相比,纯页岩含有更多的保留液体烃,具有较高量的沥青质和氮硫 - 氧(NSO)偏振的组分,表明烃排出过程相对较弱。厚纯页岩的中间部分保留了更多的液态烃,并且具有比样页的顶部和基底部分的沥青质和NSO偏振成分的百分比更高。碳氢化合物保留能力的差异被解释为主要是由砂层叠层页岩的相对较高的储层质量引起的,具有较高量的脆性矿物质和比纯页岩更大的毛孔。聚合物溶解和纳米孔吸附也是碳氢化合物保留和组分分区的关键因素。基于这项研究,我们建议桑迪层压页岩,其从邻近纯页岩接收大部分碳氢化合物,应该是目前有利的页岩勘探目标。尽管纯页岩含有高的碳氢化合物潜力,但其发展仍在等待改进的技术,这可以解决由地质条件复杂引起的挑战。

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