Journal of Jilin University(Earth Science Edition) ›› 2025, Vol. 55 ›› Issue (1): 31-45.doi: 10.13278/j.cnki.jjuese.20230115

Previous Articles     Next Articles

Comprehensive Evaluation on the Effectiveness of Conglomerate Reservoir in Shahezi Formation of Xujiaweizi Fault Depression, Songliao Basin

Gao Bo1, 2, Pan Zhejun1, Liu Lianjie2, Li Lingling2, Hong Shuxin2, Pan Huifang2, Zhang Bo2   

  1. 1. School of Earth Sciences, Northeast Petroleum University, Daqing 163318, Heilongjiang, China
    2. Exploration and Development Research Institute of Daqing Oilfield Co., Ltd., Daqing 163712, Heilongjiang, China
  • Received:2023-05-06 Online:2025-01-26 Published:2025-02-07
  • Supported by:
    the National Natural Science Foundation of China (U23A20596)  and Heilongjiang Province “Unveiling the List and Leading the Way” Science and Technology Research Project (DQYT 2022-JS-758)

Abstract: The natural gas reservoir in the deep sand and gravel strata of the Xujiaweizi fault depression in the Songliao basin is a typical unconventional resource type of “low porosity and low permeability”, with locally developed high porosity and high permeability zones, meeting the requirements for tight gas reservoir formation. Using techniques such as thin section identification, scanning electron microscopy, mercury intrusion detection, and two-dimensional nuclear magnetic resonance, an effective analysis of the sand and gravel reservoirs in the Shahezi Formation of the Xujiaweizi fault in the Songliao basin was conducted to reveal the structure of the sand and gravel reservoirs and their impact on productivity. The research results indicate that the lithology of natural gas reservoirs is mainly composed of sandstone and conglomerate, with low compositional and structural maturity. The reservoir space is mainly composed of secondary dissolution pores, and locally developed microcracks connecting pores, which improve the permeability of the reservoir; The distribution range of pore throat radius in gravel reservoirs is large (nanoscale to micrometer scale), belonging to the micropore throat type reservoir. Influenced by rock sorting, clay minerals, and the development degree of carbonates and other cementitious substances, the connectivity of pore throats in gravel reservoirs is better than that in sandstone, and that in coarse sandstone is better than that in fine sandstone. In the vertical direction, the pore throat structure of the fourth sequence is better than other sequences; The porosity of the reservoir is mainly distributed between 0.3% and 8.0%, and the permeability is mostly less than 0.987 0×10-3 μm2. Based on the empirical statistical method combining physical properties and gas production capacity, the minimum flow pore throat radius is estimated to determine the lower limit of porosity for tight sandstone as 3.0%, with a permeability of 0.019 7×10-3 μm2. The lower limit of porosity for tight conglomerate is 2.8%, and the permeability is 0.019 7×10-3 μm2.

Key words: tight reservoir, sandy conglomerate, pore structure, physical property lower limit, comprehensive evaluation; Shahezi Formation, Xujiaweizi fault depression, Songliao basin

CLC Number: 

  • P618.13
[1] Zhang Enwei, Meng Qingtao, Tang Baiqiang, Hu Fei, Dang Wei. Machine Learning-Based TOC Logging Prediction Method: A Case Study of the First Member of Qingshankou Formation in the Southern Part of Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2026, 56(3): 1062-1075.
[2] Feng Bo, Xie Yiping, Tian Hailong, Feng Guanhong, Yang Jingang.  Suitability Assessment of CO2 Geological Storage in Saline Aquifer for Central Depression of Southern Songliao Basin Based on GIS-MCDA [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(6): 1981-2000.
[3] Liu Jingyi, Chen Shoumin, Shen Zhanyong, Wang Xiaoye, Dong Xianpeng, Zhang Wen, Zhu Yushuang, .

Types of Microscopic Pore Structures in Tight Reservoirs and Effects on Seepage Characteristics:Taking Chang 6 Reservoir of Jiyuan Area in Ordos Basin as an Example [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(5): 1434-1444.

[4] Ji Jinjiao, Bian Weihua, Tang Huafeng, Li Yuanzhe, Wang Pujun. Micropore Characteristics of Tuff Lava of Yingcheng Formation in  Yingshan Fault Depression in  Songliao Basin#br# [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(4): 1051-1060.
[5] Wang Zilin, Shi Jingyue, Yang Ying, Xu Dong, Zeng Quanshu, Zhang Yichang. Pore Structure Characterization and Influencing Factors  of Fracture Conductivity in Deep Coal Rock#br# [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(4): 1061-1076.
[6] Lu Yan, Liu Zongbin, Liao Xinwu, Li Chao, Wang Ya. Fluid Flow Characteristics in Low-Permeability Sandstone Reservoirs [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(4): 1077-1090.
[7] Zhu Jianfeng, Zhang Meihua, Leng Qinglei, Liu Yuhu, Luan Ying.  Volcanic Rock Structural Fractures and Tectonic Stress Fieldsin Chaganhua Subsag, Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(3): 745-757.
[8] Wang Changdong, Hao Xiaofei, Yang Dongguang, Ning Jun, Weng Haijiao, Yan Zhaobin, Zhang Shaohua, Wu Fei. Cenozoic Diabase and Its Relation to Metallization of Sandstone Type Uranium Deposit in Southern Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(3): 775-788.
[9] Tong Lihua, Shan Xuanlong, Zhang Jiaqiang, Li Feng, Shi Lei , Li Yaohua, Xu Yinbo, Liu Yantong. Oil-Bearing Characteristics of Upper Cretaceous Oil Sands in the Dagang Area, South-Central Part of Western Slope of Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(2): 363-374.
[10] Zhang Yi, Liu Ping, Zhou Xiang. Main Controlling Factors and Distribution of Conventional and Unconventional Oil Within the 4th Member of Quantou Formation in Wangfu Area, Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(1): 46-56.
[11] Wang Ya, Liu Zongbin, Ma Kuiqian, Lu Yan, Liu Chao. Pore Structure Evaluation of Low-Permeability Sandstones Based on LDA Assisted SSOM Algorithm [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(1): 298-311.
[12] Li Yonggang.  Logging Response Characteristics of Subaqueous Eruptive Volcanic Facies of Huoshiling Formation in Chaganhua Subdepression, Changling Fault Depression [J]. Journal of Jilin University(Earth Science Edition), 2024, 54(6): 2061-2074.
[13] Wang An, Hu Mingyi, Gao Jiajun, Yang Liang, Xing Jilin. Element Geochemical Characteristics and Paleoenvironmental Significance of Mud Shale in the First Member of Qingshankou Formation of Changling Depression in Southern Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2024, 54(6): 2075-2088.
[14] Yu Zhengjun, Zhang Junhua, Zhou Hao, Ren Ruijun, Chen Yongrui, Yang Yulong. Brittleness Prediction and Evaluation of Shale Oil Reservoir in Southeastern Margin of Junggar Basin [J]. Journal of Jilin University(Earth Science Edition), 2024, 54(5): 1711-1723.
[15] Wu Yuankun, Liu Chenglin, Yu Chunyong.. Main Controlling Factors and Accumulation Mode of Deep Oil in Shuangcheng Fault Depression of Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2024, 54(5): 1443-1456.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] LIU Jian-feng, CHI Xiao-guo, ZHOU Yan, WANG Tie-fu,JIN Wei, ZHOU Jian-bo, DONG Chun-yan, LI Guang-rong. Rb-Sr Isotopic Dating of the Jinlin Pluton by Whole Rock-Hornblende Method in the Northeast Xiao Hinggan Mountains[J]. J4, 2005, 35(06): 690 -0693 .
[2] HUANG Guan-xing, SUN Ji-chao, ZHANG Ying, LIU Jing-tao, ZHANG Yu-xi, JING Ji-hong. Content and Relationship of Heavy Metals in Groundwater of Sewage Irrigation Area in Pearl River Delta[J]. J4, 2011, 41(1): 228 -234 .
[3] XIAO Chang-lai,LIANG Xiu-juan, CUI Jian-ming, LAN Ying-ying,ZHANG Jun, LI Shu-lan, LIANG Rui-qi, ZHENG Ce. Whole Curve Matching Method for Aquifer Parameters Determination[J]. J4, 2005, 35(06): 751 -0755 .
[4] GUO Zhen-hua, WANG Pu-jun, YIN Chang-hai, HUANG Yu-long. Relationship Between Lithofacies and Logging Facies of the Volcanic Reservoir Rocks in Songliao Basin[J]. J4, 2006, 36(02): 207 -0214 .
[5] SUN Yong-he, FU Xiao-fei, LV Yan-fang, FU Guang, YAN Dong. Suction Role of Seismic Pumping and Physical Simulation on Hydrocarbon Migration and Accumulation[J]. J4, 2007, 37(1): 98 -0104 .
[6] XIE Zhong-lei, CHEN Zhuo,SUN Wen-tian, YIN Bo. Content of Fluoride in Tea Leaves and Distribution of Fluoride in Soils from Different Tea Gardens[J]. J4, 2008, 38(2): 293 -0298 .
[7] JIA Jun-tao, WANG Pu-jun, SHAO Rui,CHENG Ri-hui, ZHANG Bin, HOU Jing-tao, LI Jin-long, BIAN Wei-hua. Stratigraphical Sequence and Regional Correlation of Yingcheng Formation in the Southeast of Songliao Basin[J]. J4, 2007, 37(6): 1110 -1123 .
[8] KANG Li-ming,REN Zhan-li. Study on Multi-Parameters Discrimination Method for Flow Units-Taking W93 Wellblock in Ordos Basin as An Example[J]. J4, 2008, 38(5): 749 -0756 .
[9] XUE Yong-chao, CHENG Lin-song. The Diagenetic Reservoir Facies of Chang 8 Reservoir in Baibao Oilfield[J]. J4, 2011, 41(2): 365 -371 .
[10] JIANG Ji-yi, ZHANG Yu-dong, GU Hong-biao, ZUO Lan-li. Study on the Evaluation Model of Groundwater Environment Evolution Pattern Based on Grey Correlation Entropy[J]. J4, 2009, 39(6): 1111 -1116 .