期刊
JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING
卷 204, 期 -, 页码 -出版社
ELSEVIER
DOI: 10.1016/j.petrol.2021.108610
关键词
Sichuan Basin; Qiongzhusi shale; Source rock; Hydrocarbon generation and expulsion; Resource potential
资金
- National Natural Science Foundation of China [41872148]
Significant progress has been made in exploring conventional and unconventional natural gas in the Lower Cambrian petroleum system in the Sichuan Basin, Central China. Detailed evaluation of the Qiongzhusi shale, the main source rocks in the system, has shown high potential for natural gas resources. Experimental and modeling work have provided insights into the geological and geochemical characteristics of the shale, its hydrocarbon generation and expulsion characteristics, and the potential for conventional and unconventional natural gas resources.
In recent years, significant progress and breakthroughs have been made in the exploration of conventional and unconventional natural gas in the Lower Cambrian petroleum system in the Sichuan Basin in Central China, showing excellent exploration prospects. However, detailed evaluation of the Qiongzhusi shale, the main source rocks in the Lower Cambrian petroleum system, including their hydrocarbon generation and expulsion characteristics, is lacking, even though such evaluation is critical for understanding conventional and unconventional natural gas resource potential. To investigate the geological and geochemical characteristics of the Qiongzhusi shale, experiments including pyrolysis, total organic carbon (TOC), vitrinite reflectance (Ro), gas chromatography (GC) and gas chromatography-mass spectrometry (GC-MS) were conducted. Based on modeling work and fluid inclusion analysis, the hydrocarbon generation and expulsion characteristics of the Qiongzhusi shale and their control on hydrocarbon accumulation was analyzed, and the conventional and unconventional natural gas resource potential of the Lower Cambrian petroleum system was systematically evaluated. The results indicate that the organic matter of the Qiongzhusi shale is mainly derived from bacteria and algae deposited in a saline, reducing marine environment. The shale is predominantly composed of type I kerogen with an average TOC value of 1.85 wt%, and is widely distributed in the basin with an average thickness of 212.7 m. The Qiongzhusi shale is primarily post-mature with an average vitrinite reflectance (Ro) of 2.53%. Modeling work suggests the Qiongzhusi shale reached the hydrocarbon expulsion threshold (HET) at Ro = 0.9%, and the main hydrocarbon expulsion stages are Triassic, Jurassic, and Cretaceous. The maximum hydrocarbon generation and expulsion intensities at present day are 32 x 106 t/km2 and 18 x 106 t/km2, respectively. The conventional natural gas resource potential of the Longwangmiao Formation derived from the Qiongzhusi shale is estimated to be between 9.51 x 1012 m3 and 19.03 x 1012 m3. The unconventional shale gas resource potential of the Qiongzhusi shale is predicted to be 1.4 x 1012 m3, showing significant prospects for natural gas exploration.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据