Shale gas reservoir characterisation: A typical case in the southern Sichuan Basin of China

被引:513
作者
Chen, Shangbin [1 ,2 ]
Zhu, Yanming [1 ,2 ]
Wang, Hongyan [3 ]
Liu, Honglin [3 ]
Wei, Wei [3 ]
Fang, Junhua [1 ]
机构
[1] China Univ Min & Technol, Sch Resources & Earth Sci, Xuzhou 221116, Jiangsu, Peoples R China
[2] China Univ Min & Technol, Minist Educ, Key Lab Coalbed Methane Resources & Reservoir For, Xuzhou 221116, Jiangsu, Peoples R China
[3] Petro China Explorat & Dev Res Inst, Langfang Branch, Langfang 065007, Peoples R China
基金
中国国家自然科学基金;
关键词
Shale gas; Reservoir characterisation; Southern Sichuan Basin; China; MISSISSIPPIAN BARNETT SHALE; NORTH-CENTRAL TEXAS; SOURCE ROCKS; SYSTEMS; MODEL;
D O I
10.1016/j.energy.2011.09.001
中图分类号
O414.1 [热力学];
学科分类号
070201 [理论物理];
摘要
The Lower Silurian Longmaxi Formation is an organic-rich (black) mudrock that is widely considered to be a potential shale gas reservoir in the southern Sichuan Basin (the Yangtze plate) in Southwest China. A case study is presented to characterise the shale gas reservoir using a workflow to evaluate its characteristics. A typical characterisation of a gas shale reservoir was determined using basset sample analysis (geochemical, petrographical, mineralogical, and petrophysical) through a series of tests. The results show that the Lower Silurian Longmaxi Formation shale reservoir is characterised by organic geochemistry and mineralogical, petrophysical and gas adsorption. Analysis of the data demonstrates that the reservoir properties of the rock in this region are rich and that the bottom group of the Longmaxi Formation has the greatest potential for gas production due to higher thermal maturity, total organic carbon (TOC) enrichment, better porosity and improved fracture potential. These results will provide a basis for further evaluation of the hydrocarbon potential of the Longmaxi Formation shale in the Sichuan Basin and for identifying areas with exploration potential. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:6609 / 6616
页数:8
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