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    深层-古老海相层系温压场与油气成藏

    邱楠生 刘雯 徐秋晨 刘一锋 常健

    邱楠生, 刘雯, 徐秋晨, 刘一锋, 常健, 2018. 深层-古老海相层系温压场与油气成藏. 地球科学, 43(10): 3511-3525. doi: 10.3799/dqkx.2018.286
    引用本文: 邱楠生, 刘雯, 徐秋晨, 刘一锋, 常健, 2018. 深层-古老海相层系温压场与油气成藏. 地球科学, 43(10): 3511-3525. doi: 10.3799/dqkx.2018.286
    Qiu Nansheng, Liu Wen, Xu Qiuchen, Liu Yifeng, Chang Jian, 2018. Temperature-Pressure Field and Hydrocarbon Accumulation in Deep-Ancient Marine Strata. Earth Science, 43(10): 3511-3525. doi: 10.3799/dqkx.2018.286
    Citation: Qiu Nansheng, Liu Wen, Xu Qiuchen, Liu Yifeng, Chang Jian, 2018. Temperature-Pressure Field and Hydrocarbon Accumulation in Deep-Ancient Marine Strata. Earth Science, 43(10): 3511-3525. doi: 10.3799/dqkx.2018.286

    深层-古老海相层系温压场与油气成藏

    doi: 10.3799/dqkx.2018.286
    基金项目: 

    北京市科技新星和领军人才培养计划 Z171100001117163

    国家自然科学基金项目 41690133

    国家油气重大专项 2016ZX05007-003

    详细信息
      作者简介:

      邱楠生(1968-), 男, 教授, 博士, 主要从事沉积盆地温压场研究及相关教学工作

    • 中图分类号: P618.13

    Temperature-Pressure Field and Hydrocarbon Accumulation in Deep-Ancient Marine Strata

    • 摘要: 深层海相碳酸盐岩层系尚处于勘探初期,对于海相盆地深层温压场的演化特征及主控因素认识还不够清晰.本文总结了适用于深层海相层系的温压场研究方法,并以川中古隆起震旦系气藏和塔中隆起奥陶系凝析气藏为例,展示温压场恢复的结果.川中古隆起震旦系灯影组的温度演化经历了升温-降温-快速升温-快速降温的过程,主要受大地热流与沉积埋藏史的控制;而塔中隆起奥陶系则经历了持续缓慢增温的过程,现今为最高温度.川中震旦系和塔中奥陶系现今地层压力都表现为常压,但前者经历了常压-弱超压-强超压-卸压的演化过程,而塔中隆起奥陶系在3次主要的油气成藏期没有明显的超压.对温压场的系统研究,有助于解释塔中隆起和川中古隆起现今油气相态的差异,还可以为碳酸盐岩储层高温高压模拟实验提供参数,为海相大气田进一步勘探提供理论指导.

       

    • 图  1  川中古隆起震旦系灯影组典型样品热历史反演结果

      绿色线代表可接受热史路径; 紫色线代表拟合较好热史路径; 黑色线为拟合最好热史路径

      Fig.  1.  Thermal modeling results of Dengying Formation samples in the central paleo-uplift of Sichuan Basin

      图  2  MX9井热史模拟结果

      a为MX9井埋藏史及热史; b为模拟Ro与实测Ro深度剖面; c为热流演化

      Fig.  2.  Burial history and thermal evolution of Well MX9

      图  3  川中古隆起典型井震旦系灯影组温度演化

      Temperature evolution of Dengying Formation in the central paleo-uplift of Sichuan Basin

      图  4  川中古隆起震旦系灯影组底部剩余压力演化

      Fig.  4.  Excess pressure evolution of Dengying Formation in the central paleo-uplift of Sichuan Basin

      图  5  塔中隆起典型井热流演化

      Fig.  5.  Heat flow evolution of typical wells in the central uplift of Tarim Basin

      图  6  TZ62井埋藏史、热史及两期油包裹体的捕获时期

      Fig.  6.  Burial and thermal histories of Well TZ62 and formation times for two periods' petroleum inclusions

      图  7  TZ 12井热史演化及中下奥陶统压力演化

      a为TZ12井埋藏史及热史; b为模拟Ro与实测Ro深度剖面; c为中下奥陶统压力演化

      Fig.  7.  Thermal history for Well TZ12 and pressure evolution in the O1+2 Formation

      图  8  川中古隆起震旦系天然气成藏特征与温压演化

      Fig.  8.  Evolution of temperature and pressure and characteristics of gas accumulation in the Dengying Formation of the central paleo-uplift in Sichuan Basin

      表  1  典型古老-深层海相气藏温压场特征对比

      Table  1.   Comparison of temperature and pressure in typical ancient-deep marine gas reserovirs

      温压特征 川中古隆起震旦系 塔中隆起奥陶系
      气藏相态 原油裂解气 凝析气
      现今地温 气藏温度为140~160 ℃
      地温梯度为25~30 ℃/km
      气藏温度为100~150 ℃
      地温梯度为20~24 ℃/km
      温度演化 增温-降温-快速升温-快速降温
      最大古地温超过220 ℃
      持续缓慢增温
      现今为最高温度(100~150 ℃)
      现今压力系数 1.0~1.2 0.9~1.2
      压力演化 常压-弱超压-强超压-常压 常压-弱超压
      超压成因机制 烃类生成 -
      代表井 MX9井、GS6井 TZ12井、TZ62井
      下载: 导出CSV
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