Preliminary Assessment of the Resource and Exploitation Potential of Lower Permian Marine-Continent Transitional Facies Shale Gas in the Huainan Basin, Eastern China, Based on a Comprehensive Understanding of Geological Conditions

被引:2
作者
Liu, Huihu [1 ]
Yumina, Dwi Desty [1 ]
Liu, Junlin [1 ]
Hu, Baolin [1 ]
Xu, Hongje [1 ]
Wu, Haiyan [2 ]
Shang, Jianhua [1 ]
Zheng, Kaige [1 ]
Wei, Qiang [3 ]
Zhang, Miao [1 ]
Fang, Huihuang [1 ]
机构
[1] Anhui Univ Sci & Technol, Sch Earth & Environm, Huainan 232001, Peoples R China
[2] Anhui Univ Sci & Technol, Sch Foreign Language, Huainan 232001, Peoples R China
[3] Suzhou Univ, Sch Resource & Civil Engn, Suzhou 234000, Peoples R China
基金
中国国家自然科学基金;
关键词
PORE STRUCTURE CHARACTERIZATION; NORTHEASTERN BRITISH-COLUMBIA; MISSISSIPPIAN BARNETT SHALE; NORTH-CENTRAL TEXAS; FORT-WORTH BASIN; GEOCHEMICAL CHARACTERISTICS; COALFIELD; ADSORPTION; EXPULSION; RESERVOIR;
D O I
10.1021/acsomega.1c00290
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The Huainan Basin in eastern China contains abundant shale gas resources; the Lower Permian is an exploration horizon with a high potential for shale gas in marine-continent transitional facies. However, few detailed analyses have investigated shale gas in this area. In this paper, a comprehensive investigation of the geochemical characteristics, physical properties, and gas-bearing capacities of shale reservoirs was conducted, and the resource and exploitation potential were evaluated. The results show that othe cumulative thicknesses of the Shanxi Formation (P-1s) and lower Shihezi Formation (P-2xs) are mostly greater than 35 and 65 m, respectively. The TOC contents of the P-1s and P-2xs shale vary from 0.11 to 8.87% and from 0.22 to 14.63%, respectively; the kerogens predominantly belong to type II with minor amounts of type I or type III kerogens; average R-o values range between 0.83 and 0.94% and between 0.82 and 1.02% in P-1s and P-2xs, respectively; the shale samples are primarily at a low maturity, while some shale samples have entered the high-maturity stage. The shale reservoirs have low permeability and porosity in P-1s and P-2xs, respectively. The pores of the P-1s shale reservoir are characterized by well-developed micropores and transition pores and poorly developed mesopores, while the pores in the P-2xs shale reservoir are all characterized by well-developed micropores and transition pores and some well-developed macropores; the different pore types in the shale reservoirs developed in the organic matter, clay minerals, and pyrite, while a few endogenous fractures developed in the organic matter and structural fractures developed in the minerals. The total shale gas contents in P-1s and P-2xs are 2.85 and 2.96 m(3) t(-1), respectively. The P-2xs shale reservoir has a higher hydrocarbon generation potential than P1s and has a lower gas generation potential. The total shale gas amounts in P-1s and P-2xs are 3602.29-4083.04 x 10(8) and 2811.04-3450.77 x 10(8) m(3), respectively. Further research on shale gas exploration and exploitation for these formations needs to be performed.
引用
收藏
页码:8502 / 8516
页数:15
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