Volume 45 Issue 4
Jul.  2023
Turn off MathJax
Article Contents
MOU Chunguo, XU Jie, GU Yonghong, JIA Jianpeng, WANG Wenxiong, TAN Xiucheng. Reservoir characteristics and main controlling factors of the fourth member of Ordovician Majiagou Formation in the central and eastern Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(4): 780-790. doi: 10.11781/sysydz202304780
Citation: MOU Chunguo, XU Jie, GU Yonghong, JIA Jianpeng, WANG Wenxiong, TAN Xiucheng. Reservoir characteristics and main controlling factors of the fourth member of Ordovician Majiagou Formation in the central and eastern Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(4): 780-790. doi: 10.11781/sysydz202304780

Reservoir characteristics and main controlling factors of the fourth member of Ordovician Majiagou Formation in the central and eastern Ordos Basin

doi: 10.11781/sysydz202304780
  • Received Date: 2022-11-23
  • Rev Recd Date: 2023-05-01
  • Publish Date: 2023-07-28
  • Recent exploration practice shows that the leopard porphyry dolomite reservoir in the fourth member of Ordovician Majiagou Formation in the central and eastern Ordos Basin has good exploration and development potential. Therefore, based on drilling cores, rock slices and analysis and laboratory data, the reservoir characteristics and main controlling factors of this section were analyzed. The results show that: (1) The reservoir rocks of the fourth member of Majiagou Formation mainly include leopard porphyry dolomitic limestone, leopard porphyry limy dolomite, crystalline dolomite and clotted dolomite, and the reservoir space types mainly consist of intergranular (dissolution) pores, with a small amount of lattice pores and microcracks. (2) The reservoir in the study area is generally characte-rized by low porosity and medium-low permeability pore type reservoir, in which leopard porphyry limestone dolomite and crystalline dolomite are the best reservoir rocks with wide distribution range. However, leopard porphyry dolomitic limestone is developed on a large scale, with poor reservoir performance as a whole, while clotted dolomite has good reservoir performance, but its development frequency is low. The reservoir development in the fourth member of Majiagou Formation in the central and eastern Ordos Basin is mainly controlled by sedimentary microfacies, bioturbation, dolomitization and early diagenetic karstification: as the material basis for reservoir formation, favorable sedimentary microfacies control the horizontal distribution of reservoirs; bioturbation is for dolomitization; dolomitization is the key to reservoir formation, which is conducive to the preservation of reservoir pores; early diagenetic karstification has an important contribution to the improvement of reservoir quality. In the longitudinal, the favorable reservoirs in the fourth member of Majiagou Formation are mainly located in the middle-upper part of the high-frequency upward shallowing sequence; on the plane, the favorable reservoirs are mainly concentrated in the line of Wushen Banner-Jingbian-Zhidan in the west and the two relatively independent areas of Shenmu and Mizhi in the east of the study area.

     

  • All authors disclose no relevant conflict of interests.
    The study of reservoir characteristics was carried out by MOU Chunguo and XU Jie. The reservoir genesis and main controlling factors were analyzed by GU Yonghong and JIA Jianpeng. The distribution of favorable reservoirs was predicted by WANG Wenxiong and TAN Xiucheng. The manuscript was drafted and revised by MOU Chunguo, XU Jie, and GU Yonghong. All the authors have read the last version of paper and consented for submission.
  • loading
  • [1]
    李浩. 鄂尔多斯盆地古生界气藏成藏模式及优势储层预测[J]. 特种油气藏, 2022, 29(2): 57-63. https://www.cnki.com.cn/Article/CJFDTOTAL-TZCZ202202008.htm

    LI Hao. Accumulation pattern and favorable reservoir prediction of Paleozoic gas reservoirs in Ordos Basin[J]. Special Oil & Gas Reservoirs, 2022, 29(2): 57-63. https://www.cnki.com.cn/Article/CJFDTOTAL-TZCZ202202008.htm
    [2]
    周进高, 席胜利, 邓红婴, 等. 鄂尔多斯盆地寒武系——奥陶系深层海相碳酸盐岩构造——岩相古地理特征[J]. 天然气工业, 2020, 40(2): 41-53. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202002007.htm

    ZHOU Jin'gao, XI Shengli, DENG Hongying, et al. Tectonic-lithofacies paleogeographic characteristics of Cambrian-Ordovician deep marine carbonate rocks in the Ordos Basin[J]. Natural Gas Industry, 2020, 40(2): 41-53. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202002007.htm
    [3]
    任海姣, 吴伟涛, 赵靖舟, 等. 鄂尔多斯盆地中部奥陶系马四段天然气成藏主控因素[J]. 特种油气藏, 2021, 28(2): 27-33. doi: 10.3969/j.issn.1006-6535.2021.02.004

    REN Haijiao, WU Weitao, ZHAO Jingzhou, et al. Key controlling factors of natural gas accumulation in the Ordovician Ma Member 4 in the central Ordos Basin[J]. Special Oil & Gas Reservoirs, 2021, 28(2): 27-33. doi: 10.3969/j.issn.1006-6535.2021.02.004
    [4]
    孙晓, 王杰, 陶成, 等. 鄂尔多斯盆地大牛地下古生界天然气地球化学特征及其来源综合判识[J]. 石油实验地质, 2021, 43(2): 307-314. doi: 10.11781/sysydz202102307

    SUN Xiao, WANG Jie, TAO Cheng, et al. Evaluation of geochemical characteristics and source of natural gas in Lower Paleozoic, Daniudi area, Ordos Basin[J]. Petroleum Geology & Experiment, 2021, 43(2): 307-314. doi: 10.11781/sysydz202102307
    [5]
    张威, 丁晓琪, 李春堂, 等. 鄂尔多斯盆地北部杭锦旗马家沟组四段碳酸盐岩储层分布规律[J]. 石油与天然气地质, 2021, 42(3): 615-626. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202103009.htm

    ZHANG Wei, DING Xiaoqi, LI Chuntang, et al. Distribution of paleo-karst reservoirs in Ma 4 Member, Hangjinqi area, northern Ordos Basin[J]. Oil & Gas Geology, 2021, 42(3): 615-626. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202103009.htm
    [6]
    包洪平, 杨帆, 蔡郑红, 等. 鄂尔多斯盆地奥陶系白云岩成因及白云岩储层发育特征[J]. 天然气工业, 2017, 37(1): 32-45. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201701006.htm

    BAO Hongping, YANG Fan, CAI Zhenghong, et al. Origin and reservoir characteristics of Ordovician dolostones in the Ordos Basin[J]. Natural Gas Industry, 2017, 37(1): 32-45. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201701006.htm
    [7]
    于洲, 牛小兵, 张才利, 等. 鄂尔多斯盆地米脂地区奥陶系马四段储层成因与分布[J]. 天然气工业, 2021, 41(12): 38-48. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202112005.htm

    YU Zhou, NIU Xiaobing, ZHANG Caili, et al. Genesis and distribution of reservoirs of the 4th member of Ordovician Majiagou Formation in the Mizhi area of the Ordos Basin[J]. Natural Gas Industry, 2021, 41(12): 38-48. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202112005.htm
    [8]
    任军峰, 刘新社, 喻建, 等. 鄂尔多斯盆地中东部奥陶系盐下天然气成藏特征及勘探方向[J]. 中国石油勘探, 2021, 26(6): 125-140. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY202106009.htm

    REN Junfeng, LIU Xinshe, YU Jian, et al. Characteristics of natural gas accumulation and exploration target of the Ordovician subsalt in the central and eastern Ordos Basin[J]. China Petroleum Exploration, 2021, 26(6): 125-140. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY202106009.htm
    [9]
    何发岐, 王付斌, 郭利果, 等. 鄂尔多斯盆地古生代原型盆地演化与构造沉积格局变迁[J]. 石油实验地质, 2022, 44(3): 373-384. doi: 10.11781/sysydz202203373

    HE Faqi, WANG Fubin, GUO Liguo, et al. Evolution of prototype basin and change of tectonic-sedimentary pattern in Paleozoic, Ordos Basin[J]. Petroleum Geology & Experiment, 2022, 44(3): 373-384. doi: 10.11781/sysydz202203373
    [10]
    丁晓琪, 刘鑫, 祁壮壮, 等. 碳酸盐岩孔洞型储层分层次储集空间表征: 以鄂尔多斯盆地大牛地中奥陶统马家沟组马五7为例[J]. 石油实验地质, 2021, 43(4): 689-696. doi: 10.11781/sysydz202104689

    DING Xiaoqi, LIU Xin, QI Zhuangzhuang, et al. Reservoir space characterization of vuggy carbonate reservoirs with multiple scales: a case study of Ma 5-7 interval, Middle Ordovician Majiagou Formation, Daniudi area, Ordos Basin[J]. Petroleum Geology & Experiment, 2021, 43(4): 689-696. doi: 10.11781/sysydz202104689
    [11]
    吴东旭, 喻建, 周进高, 等. 鄂尔多斯盆地奥陶系马家沟组四段沉积特征及其控储效应[J]. 古地理学报, 2021, 23(6): 1140-1157. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX202106007.htm

    WU Dongxu, YU Jian, ZHOU Jingao, et al. Sedimentary characteristics and reservoir controlling effect of the member 4 of Ordovician Majiagou Formation in Ordos Basin[J]. Journal of Palaeogeography (Chinese Edition), 2021, 23(6): 1140-1157. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX202106007.htm
    [12]
    何海清, 郭绪杰, 赵振宇, 等. 鄂尔多斯盆地奥陶系盐下马四段天然气成藏新认识及勘探重大突破[J]. 石油勘探与开发, 2022, 49(3): 429-439. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202203001.htm

    HE Haiqing, GUO Xujie, ZHAO Zhenyu, et al. New understandings on gas accumulation and major exploration breakthroughs in subsalt Ma 4 Member of Ordovician Majiagou Formation, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2022, 49(3): 429-439. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202203001.htm
    [13]
    董小波, 牛永斌. 豫西北奥陶系马家沟组三段豹斑灰岩的生物潜穴成因及成岩演化[J]. 现代地质, 2015, 29(4): 833-843. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201504011.htm

    DONG Xiaobo, NIU Yongbin. Biological burrow explanation of leopard limestone and its diagenetic evolution in the third member of Majiagou Formation in Ordovician, northwest of Henan Province[J]. Geoscience, 2015, 29(4): 833-843. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201504011.htm
    [14]
    廖慧鸿, 苏中堂, 黄文明, 等. 鄂尔多斯盆地奥陶系马家沟组五段5亚段斑化白云岩成因[J]. 石油实验地质, 2022, 44(5): 835-844. doi: 10.11781/sysydz202205835

    LIAO Huihong, SU Zhongtang, HUANG Wenming, et al. Origin of porphyry dolomite in the 5th sub-member of the 5th member of Ordovician Majiagou Formation (M55 sub-member), Ordos Basin[J]. Petroleum Geology & Experiment, 2022, 44(5): 835-844. doi: 10.11781/sysydz202205835
    [15]
    齐永安, 孟瑶, 代明月, 等. 豫西登封地区寒武系第二统朱砂洞组生物成因的豹斑构造[J]. 地质科技情报, 2014, 33(5): 1-8. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201405001.htm

    QI Yongan, MENG Yao, DAI Mingyue, et al. Biogenic leopard patch structures from the Zhushadong Formation (Cambrian series 2), Dengfeng area, western Henan[J]. Geological Science and Technology Information, 2014, 33(5): 1-8. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201405001.htm
    [16]
    BANIAK G M, GINGRAS M K, PEMBERTON S G. Reservoir characterization of burrow-associated dolomites in the Upper Devonian Wabamun Group, Pine Creek gas field, central Alberta, Canada[J]. Marine And Petroleum Geology, 2013, 48: 275-292.
    [17]
    叶禹, 李峰峰, 宋新民, 等. 生物扰动与成岩作用耦合对泥质碳酸盐岩改造机理: 以中东美索不达米亚盆地白垩系为例[J]. 石油勘探与开发, 2021, 48(6): 1187-1201. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202106011.htm

    YE Yu, LI Fengfeng, SONG Xinmin, et al. Transformation mechanism of argillaceous carbonate rock by the coupling of bioturbation and diagenesis: a case study of the Cretaceous system of the Mesopotamia Basin in the Middle East[J]. Petroleum Exploration and Development, 2021, 48(6): 1187-1201. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202106011.htm
    [18]
    钟寿康, 李凌, 谭秀成, 等. 鄂尔多斯盆地中东部马五段中粗晶白云岩成因及成岩演化[J]. 成都理工大学学报(自然科学版), 2020, 47(6): 691-710. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG202006007.htm

    ZHONG Shoukang, LI Ling, TAN Xiucheng, et al. Study on the genesis and diagenesis of medium-coarse crystal dolomite of the member 5 of Majiagou Formation in the central-eastern Ordos Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2020, 47(6): 691-710. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG202006007.htm
    [19]
    吴东旭, 吴兴宁, 王少依, 等. 鄂尔多斯盆地奥陶系颗粒滩白云岩储层特征及主控因素[J]. 海相油气地质, 2017, 22(2): 40-50. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ201702006.htm

    WU Dongxu, WU Xingning, WANG Shaoyi, et al. Characteristics and main controlling factors of Ordovician grain beach dolomite reservoir in Ordos Basin[J]. Marine Origin Petroleum Geology, 2017, 22(2): 40-50. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ201702006.htm
    [20]
    许杰, 肖笛, 苏文杰, 等. 鄂尔多斯盆地东缘奥陶系马家沟组四段豹斑状云质灰岩特征及成因: 以关家崖剖面为例[J]. 古地理学报, 2022, 24(2): 261-277. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX202202005.htm

    XU Jie, XIAO Di, SU Wenjie, et al. Characteristics and genesis of leopard-spotted dolomitic limestone in the member 4 of Ordovician Majiagou Formation: a case study from Guanjiaya section in eastern margin of Ordos Basin[J]. Journal of Palaeogeography (Chinese Edition), 2022, 24(2): 261-277. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX202202005.htm
    [21]
    XIONG Ying, TAN Xiucheng, ZUO Zhifeng, et al. Middle Ordovician multi-stage penecontemporaneous karstification in North China: implications for reservoir genesis and sea level fluctuations[J]. Journal of Asian Earth Sciences, 2019, 183: 103969.
    [22]
    谭秀成, 肖笛, 陈景山, 等. 早成岩期喀斯特化研究新进展及意义[J]. 古地理学报, 2015, 17(4): 441-456. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201504002.htm

    TAN Xiucheng, XIAO Di, CHEN Jingshan, et al. New advance and enlightenment of eogenetic karstification[J]. Journal of Palaeogeography, 2015, 17(4): 441-456. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201504002.htm
    [23]
    XIAO Di, TAN Xiucheng, XI Aihua, et al. An inland facies-controlled eogenetic karst of the carbonate reservoir in the Middle Permian Maokou Formation, southern Sichuan Basin, SW China[J]. Marine and Petroleum Geology, 2016, 72: 218-233.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(10)  / Tables(1)

    Article Metrics

    Article views (270) PDF downloads(44) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return