Enlightenment of calcite veins in deep Ordovician Wufeng–Silurian Longmaxi shales fractures to migration and enrichment of shale gas in southern Sichuan Basin, SW China

被引:0
|
作者
Cui Y. [1 ,2 ,3 ]
Li X. [1 ,2 ]
Guo W. [2 ]
Lin W. [4 ]
Hu Y. [2 ]
Han L. [5 ]
Qian C. [6 ]
Zhao J. [7 ]
机构
[1] University of Chinese Academy of Sciences, Beijing
[2] Research Center of Sichuan Basin, PetroChina Research Institute of Petroleum Exploration & Development, Beijing
[3] Petroleum Industry Press Co., Ltd., Beijing
[4] Research Institute of Digital Geology and Energy, Linyi University, Linyi
[5] MOE Key Laboratory of Continental Shale Hydrocarbon Accumulation and Efficient Development, Northeast Petroleum University, Daqing
[6] Shale Gas Exploration and Development Department, CNPC Chuanqing Drilling Engineering Co., Ltd., Chengdu
[7] PetroChina Southwest Oil & Gas Field Company, Chengdu
来源
Shiyou Kantan Yu Kaifa/Petroleum Exploration and Development | 2023年 / 50卷 / 06期
关键词
calcite vein; deep formation in southern Sichuan Basin; enrichment model; fluid inclusion; fracture; Ordovician Wufeng Formation; shale gas; Sichuan Basin; Silurian Longmaxi Formation;
D O I
10.11698/PED.20230033
中图分类号
学科分类号
摘要
The relationship between fracture calcite veins and shale gas enrichment in the deep Ordovician Wufeng Formation-Silurian Longmaxi Formation (Wufeng-Longmaxi) shales in southern Sichuan Basin was investigated through core and thin section observations, cathodoluminescence analysis, isotope geochemistry analysis, fluid inclusion testing, and basin simulation. Tectonic fracture calcite veins mainly in the undulating part of the structure and non-tectonic fracture calcite veins are mainly formed in the gentle part of the structure. The latter, mainly induced by hydrocarbon generation, occurred at the stage of peak oil and gas generation, while the former turned up with the formation of Luzhou paleouplift during the Indosinian. Under the influence of hydrocarbon generation pressurization process, fractures were opened and closed frequently, and oil and gas episodic activities are recorded by veins. The formation pressure coefficient at the maximum paleodepth exceeds 2.0. The formation uplift stage after the Late Yanshanian is the key period for shale gas migration. Shale gas migrates along the bedding to the high part of the structure. The greater the structural fluctuation is, the more intense the shale gas migration activity is, and the loss is more. The gentler the formation is, the weaker the shale gas migration activity is, and the loss is less. The shale gas enrichment in the core of gentle anticlines and gentle synclines is relatively higher. © 2023 Science Press. All rights reserved.
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页码:1199 / 1208
页数:9
相关论文
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