Volume 43 Issue 2
Mar.  2024
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LI Song, MA Liyuan, WANG Ruyue, DENG Jie, LI Yudong, QUAN Xiaoyuan, JIANG Rong. Main controlling factors and development model of tight reservoirs in the Shihezi Formation-Shanxi Formation in the Ordos Basin: Taking the Binchang area as an example[J]. Bulletin of Geological Science and Technology, 2024, 43(2): 28-40. doi: 10.19509/j.cnki.dzkq.tb20220468
Citation: LI Song, MA Liyuan, WANG Ruyue, DENG Jie, LI Yudong, QUAN Xiaoyuan, JIANG Rong. Main controlling factors and development model of tight reservoirs in the Shihezi Formation-Shanxi Formation in the Ordos Basin: Taking the Binchang area as an example[J]. Bulletin of Geological Science and Technology, 2024, 43(2): 28-40. doi: 10.19509/j.cnki.dzkq.tb20220468

Main controlling factors and development model of tight reservoirs in the Shihezi Formation-Shanxi Formation in the Ordos Basin: Taking the Binchang area as an example

doi: 10.19509/j.cnki.dzkq.tb20220468
More Information
  • Author Bio:

    LI Song, E-mail: 106155219@qq.com

  • Corresponding author: WANG Ruyue, E-mail: wry1990@vip.qq.com
  • Received Date: 28 Aug 2022
  • Accepted Date: 03 Mar 2023
  • Rev Recd Date: 21 Feb 2023
  • Objective

    Defining the distribution of sweet spots in tight reservoirs is the focus of tight oil and gas exploration.

    Methods

    Using core observation, thin section identification, X-ray diffraction, homogenization temperature measurements of inclusions, and conventional physical property analysis, the sedimentary characteristics, reservoir characteristics, and diagenesis of Upper Palaeozoic tight sandstones in the Binchang area, southern Ordos Basin were studied in detail.The main controlling factors of reservoir formation were identified and the development model of high-quality reservoirs was established.

    Results

    The results show that sedimentary facies are the basis of reservoir formation, and the core beach microfacies of the braided river delta plain have coarse grain sizes, small pore-medium-fine throat pore structures, and relatively good reservoir physical properties. The underwater distributary channel and estuary bar in front of the meandering river delta have fine grain sizes and pore throat structures of micropore-microat throat pore structure, and the reservoir's physical properties are relatively poor. Diagenesis plays an important role in controlling the development and distribution of high-quality reservoirs. Intermittent volcanic tuff is transformed into kaolinite in acidic strata and altered into chlorite sheaths in alkaline strata, which inhibits quartz overgrowth and calcite cementation and protects the reservoir space. The secondary enlargement of quartz is mainly caused by the leaching of SiO2 from mudstone to sandstone.The main reasons for the cementation of calcite roof and floor are the filling of feldspar and the dissolution of cuttings in the middle and late stages of calcite. The microfractures formed by late tectonic transformation have no calcite cementation, which improves the physical properties of the reservoir and plays an adjusting role in the gas reservoir. There are two solution pore development zones near burial depths of 3 750 m and 3 900 m in the Binchang area. The optimal reservoir is the medium-coarse-grained sandstone rich in chlorite mantle formed by the transformation of volcanic tuffaceous matter in the dissolution pore development zone. The sub-optimal reservoir is mainly distributed in the middle and lower parts of the sand body with a greater single-body thickness, cyclicity and no mudstone interval in the dissolution pore development zone.This zone is composed mainly of medium-coarse-grained sandstone lacking chlorite film, calcite cementation and secondary enlargement of quartz are the lowest.

    Conclusion

    These research results further increase the understanding of the genesis of the development of high-quality tight sandstone reservoirs in the Upper Palaeozoic, providing important guidance for natural gas exploration and development in this area.

     

  • The authors declare that no competing interests exist.
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  • [1]
    付金华, 魏新善, 任军峰, 等. 伊陕斜坡上古生界大面积岩性气藏分布与成因[J]. 石油勘探与开发, 2008, 35(6): 664-667. doi: 10.3321/j.issn:1000-0747.2008.06.004

    FU J H, WEI X S, REN J F, et al. Distribution and genesis of lare-scale Upper Palaeozoic lithologic gas reservoirs on Yi-Shan Slope[J]. Petroleum Exploration and Development, 2008, 35(6): 664-667. (in Chinese with English abstract) doi: 10.3321/j.issn:1000-0747.2008.06.004
    [2]
    杨华, 付金华, 魏新善, 等. 鄂尔多斯盆地天然气成藏特征[J]. 天然气工业, 2005, 25(4): 9-11. doi: 10.3321/j.issn:1000-0976.2005.04.003

    YANG H, FU J H, WEI X S, et al. Charcateristics of natural gas reservoir formation in Ordos Basin[J]. Natural Gas Industry, 2005, 25(4): 9-11. (in Chinese with English abstract) doi: 10.3321/j.issn:1000-0976.2005.04.003
    [3]
    丁晓琪, 张哨楠, 周文, 等. 鄂尔多斯盆地北部上古生界致密砂岩储层特征及其成因讨论[J]. 石油与天然气地质, 2007, 28(4): 491-496. doi: 10.3321/j.issn:0253-9985.2007.04.008

    DING X Q, ZHANG S N, ZHOU W, et al. Characteristics and genesis of the Upper Paleozoic tight sandstone reservoirs in the northern Ordos Basin[J]. Oil & Gas Geology, 2007, 28(4): 491-496. (in Chinese with English abstract) doi: 10.3321/j.issn:0253-9985.2007.04.008
    [4]
    张哨楠. 致密天然气砂岩储层: 成因和讨论[J]. 石油与天然气地质, 2008, 29(1): 1-11. doi: 10.3321/j.issn:0253-9985.2008.01.001

    ZHANG S N. Tight sandstone gas reservoirs: Their origin and discussion[J]. Oil & Gas Geology, 2008, 29(1): 1-11. (in Chinese with English abstract) doi: 10.3321/j.issn:0253-9985.2008.01.001
    [5]
    付金华, 魏新善, 南珺祥, 等. 鄂尔多斯盆地上古生界致密砂岩气田储集层特征与成因[J]. 古地理学报, 2013, 15(8): 529-538. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201304011.htm

    FU J H, WEI X S, NAN J X, et al. Characteristics and origin of reservoirs of gas fields in the Upper Paleozoic tight sandstone, Ordos Basin[J]. Journal of Palaeogeography, 2013, 15(8): 529-538. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201304011.htm
    [6]
    琚慧娇. 苏里格气田西区苏48区上古生界储层特征及其主控因素研究[D]. 西安: 西北大学, 2011: 95-101.

    JU H J. The characteristics of Upper Paleozoic reservoir in Sulige gasfield and its main control factors[D]. Xi'an: Northwest University, 2011: 95-101. (in Chinese with English abstract)
    [7]
    刘喜杰, 马尊敬, 韩冬, 等. 鄂尔多斯盆地东缘临兴区块致密砂岩优质储层形成的主控因素[J]. 天然气地球科学, 2018, 29(4): 481-490. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201804004.htm

    LIU X J, MA Z J, HAN D, et al. Research on the main factors of high quality tight sandstone reservoir in Linxing block, Ordos Basin[J]. Natural Gas Geoscience, 2018, 29(4);481-490. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201804004.htm
    [8]
    王翀峘, 魏钦廉, 胡榕, 等. 不同物源体系致密储层微观结构特征及成因分析: 以陇东地区樊家川和南梁长6段为例[J]. 地质科技通报, 2023, 42(1): 286-298. doi: 10.19509/j.cnki.dzkq.2021.0258

    WANG C H, WEI Q L, HU R, et al. Microstructure charateristics and genetic analysis of tight reservoirs with different provenance systems: A case study of Fanjiachuan and Nanliang region of Chang 6 reservoir in Longdong area, Ordos Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(1): 286-298. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2021.0258
    [9]
    尹相东, 蒋恕, 吴鹏, 等. 致密砂岩酸性和碱性成岩环境特征及对储层物性的控制: 以鄂尔多斯盆地临兴和神府地区为例[J]. 地质科技通报, 2021, 40(1): 142-151. doi: 10.19509/j.cnki.dzkq.2021.0109

    YIN X D, JIANG S, WU P, et al. Features of the acid and alkaline diagenetic environment of tight sandstones and the control of the reservoir physical properties: A case study of the Linxing and Shenfu district, eastern Ordos Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(1): 142-151. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2021.0109
    [10]
    ZHAO Y, WANG W, GUO R, et al. Relation of heterogeneity and gas-bearing capacity of tight sandstone: A case study of the Upper Paleozoic tight gas sandstone reservoir in the southeast of the Ordos Basin[J]. ACS Omega, 2021, 6(24): 15716-15726. doi: 10.1021/acsomega.1c00965
    [11]
    WU H, GUO M, ZHAO J, et al. Densification mechanisms of tight sandstones in closed to semi-closed systems: Typical example from the Upper Paleozoic in the Linxing area, Ordos Basin[J]. Arabian Journal of Geosciences, 2021, 14: 1167.1-1167.18.
    [12]
    曲希玉, 苗长盛, 李瑞磊, 等. 致密砂岩储层物性影响因素及优质储层主控因素: 以松辽盆地长岭断陷龙凤山次凹营城组为例[J]. 天然气地球科学, 2022, 33(7): 1036-1048. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202207002.htm

    QU X Y, MIAO C S, LI R L, et al. Influencing factors of tight clastic reservoir physical properties and main controlling factors of high-quality reservoirs: Taking the Yingcheng Formation of Longfengshan Sub-sag in Changling Fault Depression of Songliao Basin as an example[J]. Natural Gas Geoscience, 2022, 33(7): 1036-1048. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202207002.htm
    [13]
    LI Y, FAN A, YANG R, et al. Braided deltas and diagenetic control on tight sandstone reservoirs: A case study on the Permian Lower Shihezi Formation in the southern Ordos Basin(central China)[J]. Sedimentary Geology, 2022, 435: 106156.1-106156.16.
    [14]
    WANG R, LIU K, SHI W, et al. Reservoir densification, pressure evolution, and natural gas accumulation in the Upper Paleozoic tight sandstones in the north Ordos Basin, China[J]. Energies, 2022, 15(6): 1990.1-1990.21.
    [15]
    周进松, 乔向阳, 王若谷, 等. 鄂尔多斯盆地延安气田山西组致密砂岩气有效储层发育模式[J]. 天然气地球科学, 2022, 33(2): 195-206. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202202002.htm

    ZHOU J S, QIAO X Y, WANG R G, et al. Effective reservoir development model of tight sandstone gas in Shanxi Formation of Yan'an gas field, Ordos Basin[J]. Natural Gas Geoscience, 2022, 33(2): 195-206. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202202002.htm
    [16]
    付金华, 郑聪斌. 鄂尔多斯盆地奥陶纪华北海和祁连海演变及岩相古地理特征[J]. 古地理学报, 2001, 3(4): 25-34. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200104002.htm

    FU J H, ZHENG C B. Evolution between North China Sea and Qilian Sea of the Ordovician and the characteristics of lithofacies palaeogeography in Ordos Basin[J]. Journal of Palaeogeography, 2001, 3(4): 25-34. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200104002.htm
    [17]
    陈孟晋, 汪泽成, 郭彦如, 等. 鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力[J]. 石油勘探与开发, 2006, 33(1): 1-5. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200601000.htm

    CHEN M J, WANG Z C, GUO Y R, et al. Late Paleozoic sedimentary system and gas potential in the south Ordos Basin[J]. Petroleum Exploration and Development, 2006, 33(1): 1-5. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200601000.htm
    [18]
    赵谦平, 王若谷, 高飞, 等. 鄂尔多斯盆地东南部延长探区上古生界物源分析[J]. 西北大学学报(自然科学版), 2015, 45(6): 933-941. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ201506012.htm

    ZHAO Q P, WANG R G, Gao F, et al. Provenance analysis of Upper Paleozoic in Yanchang Blocks, the southeast Ordos Basin[J]. Journal of Northwest University(Natural Science Edition), 2015, 45(6): 933-941. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ201506012.htm
    [19]
    于兴河, 王香增, 王念喜, 等. 鄂尔多斯盆地东南部上古生界层序地层格架及含气砂体沉积演化特征[J]. 古地理学报, 2017, 19(6): 935-954. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201706001.htm

    YU X H, WANG X Z, WANG N X, et al. Sequence stratigraphic framework and sedimentary evolution characteristics of gas-bearing sandbody in the Upper Paleozoic in southeastern Ordos Basin[J]. Journal of Palaeogeography, 2017, 19(6): 935-954. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201706001.htm
    [20]
    屈红军, 马强, 高胜利, 等. 物源与沉积相对鄂尔多斯盆地东南部上古生界砂体展布的控制[J]. 沉积学报, 2011, 29(5): 825-834. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201105003.htm

    QU H J, MA Q, GAO S L, et al. Controls of provenance and depositional facies on sandbody distributions of the Upper Paleozoic in southeast Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(5): 825-834. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201105003.htm
    [21]
    王香增, 周进松. 鄂尔多斯盆地东南部下二叠统山西组二段物源体系及沉积演化模式[J]. 天然气工业, 2017, 37(11): 9-17. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201711005.htm

    WANG X Z, ZHOU J S. Provenance system and sedimentary evolution model of the Second Member of Lower Permian Shanxi Formation in the southeastern Ordos Basin[J]. Natural Gas Industry, 2017, 37(11): 9-17. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201711005.htm
    [22]
    李智, 叶加仁, 曹强, 等. 鄂尔多斯盆地杭锦旗独贵加汗区带下石盒子组储层特征及孔隙演化[J]. 地质科技通报, 2021, 40(4): 49-60. doi: 10.19509/j.cnki.dzkq.2021.0404

    LI Z, YE J R, CAO Q, et al. Reservoir characteristics and pore evolution of the Lower Shihezi Formation in Duguijiahan zone, Hangjinqi area, Ordos Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(4): 49-60. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2021.0404
    [23]
    黎盼, 孙卫, 高永利, 等. 致密砂岩储层差异性成岩演化对孔隙度定量演化表征影响: 以鄂尔多斯盆地马岭地区长81储层为例[J]. 地质科技情报, 2018, 37(1): 135-142. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201801018.htm

    LI P, SUN W, GAO Y L, et al. Quantitative calculation of tight sandstone reservoir porosity evolution based on different diagenesis: A case study from Chang 81 reservoir of Maling area, Ordos Basin[J]. Geological Science and Technology Information, 2018, 37(1): 135-142. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201801018.htm
    [24]
    王瑞飞, 王立新, 李俊鹿, 等. 浅层致密砂岩油藏成岩作用及孔隙演化[J]. 地球物理学进展, 2020, 35(4): 1465-1470. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ202004030.htm

    WANG R F, WANG L X, LI J L, et al. Diagenesis and porosity evolution of ultra-low permeability and shallow layers sandstone reservoir[J]. Progress in Geophysics, 2020, 35(4): 1465-1470. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ202004030.htm
    [25]
    郑浚茂, 庞明. 石英砂岩的硅质胶结作用及其对储集性能的影响[J]. 沉积学报, 1988, 6(1): 29-39. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198801003.htm

    ZHENG J M, PANG M. Quartzcementaion in quarzose sandstone and its influence on sandstone porosity[J]. Acta Sedimentologica Sinica, 1988, 6(1): 29-39. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198801003.htm
    [26]
    贾珍臻, 林承焰, 任丽华, 等. 苏德尔特油田低渗透凝灰质砂岩成岩作用及储层质量差异性演化[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1624-1636. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201606003.htm

    JIA Z Z, LIN C Y, REN L H, et al. Diagenesis and reservoir quality evolution of low permeability tuffaceous sandstones in Suderte oilfield[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(6): 1624-1636. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201606003.htm
    [27]
    田建锋, 喻建, 张志国, 等. 砂岩中碱性溶蚀研究进展[J]. 地质科技通报, 2022, 41(5);83-93. doi: 10.19509/j.cnki.dzkq.2022.0195

    TIAN J F, YU J, ZHANG Z G, et al. Advance in alkaline dissolution of sandstone[J]. Bulletin of Geological Science and Technology, 2022, 41(5): 83-93. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0195
    [28]
    黄思静, 黄可可, 冯文立, 等. 成岩过程中长石、高岭石、伊利石之间的物质交换与次生孔隙的形成: 来自鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究[J]. 地球化学, 2009, 38(5): 498-506. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200905010.htm

    HUANG S J, HUANG K K, FENG W L, et al. Mass exchanges among feldspar, kaolinite and illite and their influences on secondary porosity formation in clastic diagenesis: A case study on the Upper Paleozoic, Ordos Basin and Xujiahe Formation, western Sichuan Depression[J]. Geochimica, 2009, 38(5): 498-506. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200905010.htm
    [29]
    王行信, 周书欣. 泥岩成岩作用对砂岩储层胶结作用的影响[J]. 石油学报, 1992, 13(4): 20-30. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199204003.htm

    WANG X X, ZHOU S X. The effect of diagenesis of mudstone on the cementation of a sandstone reservoir[J]. Acta Petrolei Sinica, 1992, 13(4);20-30. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199204003.htm
    [30]
    闫建萍, 刘池洋, 张卫刚, 等. 鄂尔多斯盆地南部上古生界低孔低渗砂岩储层成岩作用特征研究[J]. 地质学报, 2010, 84(2): 272-279. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201002013.htm

    YAN J P, LIU C Y, ZHANG W G, et al. Diagenetic characteristics of the lower porosity and permeability sandstones of the Upper Paleozoic in the south of Ordos Basin[J]. Acta Geologogica Sinica, 2010, 84(2): 272-279. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201002013.htm
    [31]
    斯尚华, 赵靖舟, 蒙启安, 等. 三肇凹陷扶余油层方解石胶结物特征及其对储层致密化的影响[J]. 油气地质与采收率, 2018, 25(2): 58-63. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS201802009.htm

    SI S H, ZHAO J Z, MENG Q A, et al. Characteristics of calcite cement and its influence on reservoir densification in Fuyu oil reservoir of Sanzhao Sag[J]. Petroleum Geology and Recovery Efficiency, 2018, 25(2): 58-63. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS201802009.htm
    [32]
    黄思静, 黄可可, 张雪花, 等. 碳酸盐倒退溶解模式的化学热力学基础: 与CO2有关的溶解介质[J]. 成都理工大学学报(自然科学版), 2009, 36(5): 457-464. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200905001.htm

    HUANG S J, HUANG K K, ZHANG X H, et al. Chemical thermodynamics foundation of retrograde solubility for carbonate: Solution media related to CO2[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 2009, 36(5): 457-464. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200905001.htm
    [33]
    史基安, 晋慧娟, 薛莲花. 长石砂岩中长石溶解作用发育机理及其影响因素分析[J]. 沉积学报, 1994, 12(3): 65-75. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB403.007.htm

    SHI J A, JIN H J, XUE L H. Analysis on mechanism of feldspar dissolution and its influencing factors in feldspar-rich sandstone reservoir[J]. Acta Sedimentol Sinica, 1994, 12(3): 65-75. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB403.007.htm
    [34]
    STEFANSSON A. Dissolution of Primary minerals of basalt in natural waters: I. Calculation of mineral solubilities from 0℃ to 350℃[J]. Chem. Geol., 2001, 172(3/4): 225-250.
    [35]
    李松, 刘玲, 吴疆, 等. 鄂尔多斯盆地南部山西组-下石盒子组致密砂岩成岩演化[J]. 天然气地球科学, 2021, 32(1): 47-56. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202101006.htm

    LI S, LIU L, WU J, et al. Diagenetic evolution of tight sandstone of Shanxi-Lower Shihezi formations in the southern Ordos Basin[J]. Natural Gas Geoscience, 2021, 32(1): 47-56. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202101006.htm
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