Petroleum Science >2019,??Issue 2:??285-297 DOI: https://doi.org/10.1007/s12182-019-0307-9
Sedimentary and geochemical characteristics of the Triassic Chang 7 Member shale in the Southeastern Ordos Basin, Central China
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文章信息
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作者：Jing?Wei Cui, Ru?Kai Zhu, Zhong Luo and Sen Li
作者單位：Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China; Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, Shandong University of Science and Technology, Qingdao 266590, Shandong, China,Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China,Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China and Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China
投稿時(shí)間：2018-11-29
引用方式：Cui, JW., Zhu, RK., Luo, Z. et al. Pet. Sci. (2019) 16: 285. https://doi.org/10.1007/s12182-019-0307-9
文章摘要
The Ordos Basin is the largest petroliferous basin in China, where the Chang 7 Member shale serves as the major source rock in the basin, with an area of more than 100,000 km2. So far, sedimentary and geochemical characterizations have rarely been conducted on the shale in shallow (< 1000 m) areas in the southeastern part of the basin, but such characterizations can help identify the genesis of organic-rich shale and promote the prediction and recovery of shale oil. In this paper, several outcrop sections of the Chang 7 Member in the Tongchuan area were observed and sampled, and sedimentary and geochemical characterizations were conducted for the well-outcropped YSC section. The study results show that the Chang 7 Member shale is widely distributed laterally with variable thickness. The organic-rich shale is 7–25 m thick in total and exhibits obvious horizontal variation in mineral composition. In the eastern sections, the shale contains organic matter of Type II2– III and is low in thermal maturity, with high clay mineral content, low K-feldspar content, and no pyrite. In the western sections, the shale contains Type II1 organic matter and is low in thermal maturity, with high clay mineral, K-feldspar, and pyrite contents. The YSC section reveals three obvious intervals in vertical mineral composition and organic abundance. The Chang 7 Member organic-rich shale (TOC > 10%) contains mainly sapropelite and liptinite, with Type II kerogen. It is generally characterized by a hydrocarbon potential of more than 70 mg/g, low maturity, and shallow–semideep lacustrine facies. In the western sections, the shale, still in a low maturity stage, has a higher hydrocarbon potential and is optional for shale oil recovery. However, the Chang 7 Member shale in the study area is highly heterogeneous and its shale oil recovery is practical only in the organic-rich intervals.
