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    东海盆地丽水凹陷CO2分布特征及成藏主控因素

    牛杏 何云龙 庄新国

    牛杏, 何云龙, 庄新国, 2021. 东海盆地丽水凹陷CO2分布特征及成藏主控因素. 地球科学, 46(10): 3549-3559. doi: 10.3799/dqkx.2021.021
    引用本文: 牛杏, 何云龙, 庄新国, 2021. 东海盆地丽水凹陷CO2分布特征及成藏主控因素. 地球科学, 46(10): 3549-3559. doi: 10.3799/dqkx.2021.021
    Niu Xing, He Yunlong, Zhuang Xinguo, 2021. Distribution and Major Controlling Factors of CO2 Reservoirs in Lishui Sag, East China Sea Basin. Earth Science, 46(10): 3549-3559. doi: 10.3799/dqkx.2021.021
    Citation: Niu Xing, He Yunlong, Zhuang Xinguo, 2021. Distribution and Major Controlling Factors of CO2 Reservoirs in Lishui Sag, East China Sea Basin. Earth Science, 46(10): 3549-3559. doi: 10.3799/dqkx.2021.021

    东海盆地丽水凹陷CO2分布特征及成藏主控因素

    doi: 10.3799/dqkx.2021.021
    基金项目: 

    “十三五”国家重大科技专项 2016ZX05027-001-006

    详细信息
      作者简介:

      牛杏(1989-), 女, 讲师, 主要从事油气成藏、地球化学、沉积学方面的研究.ORCID: 0000-0001-7947-7984.E-mail: xingncug@163.com

      通讯作者:

      何云龙, Email: ylhe@cug.edu.cn

    • 中图分类号: P62

    Distribution and Major Controlling Factors of CO2 Reservoirs in Lishui Sag, East China Sea Basin

    • 摘要: 基于丽水凹陷钻井和地震资料,综合天然气地球化学参数、基底断裂和岩浆底辟发育特征等,研究丽水凹陷CO2的分布特征及其成藏主控因素.研究结果表明,丽水凹陷CO2纵向上主要分布在灵峰组、明月峰组下段及元古界基底片麻岩中,不同层位CO2的含量差别很大;平面上,温州13-1、丽水35-7和南平5-2 CO2气藏均位于岩浆底辟体之上或者附近,同时周围亦发育断层,而丽水36-1高含CO2气藏和LF-1井含CO2气藏周围底辟不发育,均紧邻灵峰凸起西侧的控洼断裂.丽水凹陷幔源CO2成藏主要受早中新世和晚中新世两期火山岩浆活动的影响,这两期火山活动将幔源CO2带到地壳浅层,通过砂体侧向输导进入有利圈闭聚集成藏.

       

    • 图  1  丽水凹陷构造单元划分及基底断裂平面分布

      Fig.  1.  Plane distribution of basement faults and tectonic units in Lishui sag

      图  2  丽水凹陷地层及构造演化

      仝志刚等(2012)张田等(2015)蒋一鸣等(2020)修编

      Fig.  2.  Stratigraphic and tectonic evolution of Lishui sag

      图  3  丽水凹陷CO2有机与无机成因判别

      图据戴金星等(1995)

      Fig.  3.  Identification of organic or inorganic origin of CO2 in Lishui sag

      图  4  丽水凹陷(含)CO2井与基底断裂、岩浆底辟

      Fig.  4.  The positions of wells containing CO2 and plane distribution of basement faults and magmatic diapers

      图  5  灵峰凸起西侧深断裂详细解剖

      Fig.  5.  Detailed analysis of deep faults on the west side of Lingfeng uplift

      图  6  灵峰凸起西侧深断裂的活动性

      Fig.  6.  The activity of deep faults on the west side of Lingfeng uplift

      图  7  南平5-2构造及温州13-1构造CO2气藏地震剖面解析

      图例同图 5

      Fig.  7.  Seismic section analysis of Nanping 5-2 and Wenzhou 13-1 structure CO2 gas reservoirs

      图  8  南平5-2构造紧邻断层活动速率

      Fig.  8.  Activity rate of faults adjacent to Nanping 5-2 structure

      表  1  丽水凹陷天然气地球化学参数

      Table  1.   Geochemical parameters of natural gas in Lishui sag

      井名 地层 深度(m) 气体主要组分(%) 碳同位素(‰) R/Ra 3He/ 4He(10-7) 数据来源
      CH4 C2+ N2 CO2 δ13CCO2
      SMT-1 E1l 2 571~2 589 1.62 0.85 0.67 95.63 -4.15 苏奥等,2014
      何家雄等,2005
      黄志龙等,2003
      2 638~2 657 0.42 - 0.29 99.42 -4.19
      WZ13-1-1 E1l 3 335~3 345 4.76 0.76 94.47 -4.00 7.20 101.00
      3 405~3 412 1.19 0.22 98.59 -4.20 8.80 123.00
      3 641~3 666 0.13 99.87 -4.20 5.40 75.00
      LS36-1-1 E1m 2 251~2 283 55.45 6.85 3.55 34.15 -5.03
      55.10 6.75 3.44 34.50 -4.67
      LF-1 基底 2 511~2 530 59.48 6.16 痕量 -22.20 苏奥等,2014
      黄志龙等,2003
      葛和平等,2007
      LS36-1-2 E1m2 2 238~2 260 56.52 10.68 1.06 31.74 -4.60 8.80 59.70
      下载: 导出CSV
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