Geological-petrophysical insights in the deep Cambrian dolostone reservoirs in Tarim Basin, China

被引:46
作者
Lai, Jin [1 ,2 ]
Liu, Shichen [1 ]
Xin, Yi [3 ]
Wang, Song [1 ]
Xiao, Chengwen [3 ]
Song, Qiuqiang [3 ]
Chen, Xu [3 ]
Yang, Kefu [3 ]
Wang, Guiwen [1 ,2 ]
Ding, Xiujian [4 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing, Peoples R China
[2] China Univ Petr, Coll Geosci, Beijing, Peoples R China
[3] China Natl Petr Corp CNPC, Tarim Oilfield Co, Res Inst Petr Explorat & Dev, Xinjiang, Peoples R China
[4] China Univ Petr East China, Key Lab Deep Oil & Gas, Qingdao, Peoples R China
关键词
THERMOCHEMICAL SULFATE REDUCTION; ORDOVICIAN CARBONATE RESERVOIRS; TRIASSIC YANCHANG FORMATION; TAHE OIL-FIELD; ORDOS BASIN; NW CHINA; SICHUAN BASIN; DOLOMITE RESERVOIRS; TAZHONG UPLIFT; IMAGE LOGS;
D O I
10.1306/03122119135
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Cores, thin sections, and cathodoluminescence analysis were integrated to document the occurrence and petrology of dolomites, and their pore systems in the Cambrian of Tarim Basin, China. Depositional facies, pore types, and dolomitization processes of various dolostone reservoir types are determined. Six types of dolomite are recognized, including microbial dolomite, dolomicrite, fabric retentive dolomite, fabric-obliterative dolomite, fine to medium crystalline dolomite cement, and saddle dolomite cement. Pore systems are dominantly vugs, anhydrite dissolution pores, intercrystalline pores, intercrystalline dissolution pores, fabric dissolution pores, and microfractures. Four porous dolostone reservoirs include sabkha dolostone, seepage-reflux dolostone, burial dolostone, and hydrothermal dolostone. Fractures are an important factor in enhancing reservoir quality in dolostone reservoirs. Conventional wire-line logs and image logs are calibrated with cores and related thin sections. Sabkha dolostone reservoirs are characterized by dark and bright spots on the image logs. Seepage-reflux dolostone reservoirs are related to high-energy depositional facies and are characterized by low gamma-ray amplitude, increasing sonic transit time and neutron porosity but reducing bulk density values. Evident dark spots (vugs) are recognized on image logs, and all three porosity logs suggest relatively high reservoir quality in burial dolostone reservoirs. Hydrothermal dolostone reservoirs are recognized by high gamma-ray response caused by hydrothermal minerals (fluorite), and porosity curves indicate good reservoir quality, which is supported by dark spots (vugs) on the image logs. Rapid decrease in resistivity, increasing in sonic transit time values, and the dark sinusoidal waves on the image logs are typical of fractured dolostone reservoirs. The distribution of dolostone reservoirs in each well is predicted using a comprehensive analysis of conventional and image logs, and they are calibrated with oil test data. The research provides insights in the analysis of genetic model of deeply buried dolostone reservoirs and establishes the predictable model for reservoir quality in dolostones via well logs.
引用
收藏
页码:2263 / 2296
页数:34
相关论文
共 94 条
  • [1] Reservoir heterogeneity and fracture parameter determination using electrical image logs and petrophysical data (a case study, carbonate Asmari Formation, Zagros Basin, SW Iran)
    Aghli, Ghasem
    Moussavi-Harami, Reza
    Mohammadian, Ruhangiz
    [J]. PETROLEUM SCIENCE, 2020, 17 (01) : 51 - 69
  • [2] Fractured zones detection using conventional petrophysical logs by differentiation method and its correlation with image logs
    Aghli, Ghasem
    Soleimani, Bahman
    Moussavi-Harami, Reza
    Mohammadian, Ruhangiz
    [J]. JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING, 2016, 142 : 152 - 162
  • [3] Multiple fluid flow events and the formation of saddle dolomite: case studies from the Middle Devonian of the Western Canada Sedimentary Basin
    Al-Aasm, IS
    Lonnee, J
    Clarke, J
    [J]. MARINE AND PETROLEUM GEOLOGY, 2002, 19 (03) : 209 - 217
  • [4] Effects of progressive burial on matrix porosity and permeability of dolostones in the foreland basin of the Alpine Orogen, Switzerland
    Aschwanden, Lukas
    Diamond, Larryn W.
    Adams, Arthur
    [J]. MARINE AND PETROLEUM GEOLOGY, 2019, 100 : 148 - 164
  • [5] Origin of dolomite in the Middle Ordovician peritidal platform carbonates in the northern Ordos Basin, western China
    Bai, Xiao-Liang
    Zhang, Shao-Nan
    Huang, Qing-Yu
    Ding, Xiao-Qi
    Zhang, Si-Yang
    [J]. PETROLEUM SCIENCE, 2016, 13 (03) : 434 - 449
  • [6] The use of microresistivity image logs for facies interpretations: An example in point-bar deposits of the McMurray Formation, Alberta, Canada
    Brekke, Howard
    MacEachern, James A.
    Roenitz, Tania
    Dastgard, Shahin E.
    [J]. AAPG BULLETIN, 2017, 101 (05) : 655 - 682
  • [7] Thermochemical sulphate reduction in Cambro-Ordovician carbonates in Central Tarim
    Cai, CF
    Hu, WS
    Worden, RH
    [J]. MARINE AND PETROLEUM GEOLOGY, 2001, 18 (06) : 729 - 741
  • [8] Application of sulfur and carbon isotopes to oil-source rock correlation: A case study from the Tazhong area, Tarim Basin, China
    Cai, Chunfang
    Zhang, Chunming
    Worden, Richard H.
    Wang, Tiankai
    Li, Hongxia
    Jiang, Lei
    Huang, Shaoying
    Zhang, Baoshou
    [J]. ORGANIC GEOCHEMISTRY, 2015, 83-84 : 140 - 152
  • [9] Chen JF, 2000, AAPG BULL, V84, P591
  • [10] Hydrothermal alteration of dolostones in the Lower Ordovician, Tarim Basin, NW China: Multiple constraints from petrology, isotope geochemistry and fluid inclusion microthermometry
    Dong, Shaofeng
    Chen, Daizhao
    Ling, Hairuo
    Zhou, Xiqiang
    Wang, Dan
    Guo, Zenghui
    Jiang, Maosheng
    Qian, Yixiong
    [J]. MARINE AND PETROLEUM GEOLOGY, 2013, 46 : 270 - 286