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
来源
ACS OMEGA | 2021年 / 6卷 / 12期
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
相关论文
共 44 条
  • [1] Bordenave M. L, 1993, APPL PETROLEUM GEOCH, P237
  • [2] Barnett Shale gas production, Fort Worth Basin: Issues and discussion
    Bowker, Kent A.
    [J]. AAPG BULLETIN, 2007, 91 (04) : 523 - 533
  • [3] Methodology of coalbed methane resource assessment
    Boyer, CM
    Bai, QZ
    [J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY, 1998, 35 (1-4) : 349 - 368
  • [4] Fractal characteristics of pores in non-marine shales from the Huainan coalfield, eastern China
    Bu, Honglin
    Ju, Yiwen
    Tan, Jingqiang
    Wang, Guochang
    Li, Xiaoshi
    [J]. JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING, 2015, 24 : 166 - 177
  • [5] Carbon and hydrogen isotopic reversals in deep basin gas: Evidence for limits to the stability of hydrocarbons
    Burruss, R. C.
    Laughrey, C. D.
    [J]. ORGANIC GEOCHEMISTRY, 2010, 41 (12) : 1285 - 1296
  • [6] Bustin R.M., 2005, American Association of Petroleum Geologists explorer, V26, P5
  • [7] Determining gas expulsion vs retention during hydrocarbon generation in the Eagle Ford Shale using noble gases
    Byrne, D. J.
    Barry, P. H.
    Lawson, M.
    Ballentine, C. J.
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2018, 241 : 240 - 254
  • [8] The organic matter distribution and methane capacity of the lower Cretaceous strata of northeastern British Columbia, Canada
    Chalmers, Gareth R. L.
    Bustin, R. Marc
    [J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY, 2007, 70 (1-3) : 223 - 239
  • [9] Lower Cretaceous gas shales in northeastern British Columbia, Part II: evaluation of regional potential gas resources
    Chalmers, Gareth R. L.
    Bustin, R. Marc
    [J]. BULLETIN OF CANADIAN PETROLEUM GEOLOGY, 2008, 56 (01) : 22 - 61
  • [10] Pore structure characterization of North American shale gas reservoirs using USANS/SANS, gas adsorption, and mercury intrusion
    Clarkson, C. R.
    Solano, N.
    Bustin, R. M.
    Bustin, A. M. M.
    Chalmers, G. R. L.
    He, L.
    Melnichenko, Y. B.
    Radlinski, A. P.
    Blach, T. P.
    [J]. FUEL, 2013, 103 : 606 - 616