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    查干凹陷中、新生代热史及烃源岩热演化

    左银辉 马维民 邓已寻 郝情情 李新军 郭俊梅 冉庆 汪立蓉

    左银辉, 马维民, 邓已寻, 郝情情, 李新军, 郭俊梅, 冉庆, 汪立蓉, 2013. 查干凹陷中、新生代热史及烃源岩热演化. 地球科学, 38(3): 553-560. doi: 10.3799/dqkx.2013.055
    引用本文: 左银辉, 马维民, 邓已寻, 郝情情, 李新军, 郭俊梅, 冉庆, 汪立蓉, 2013. 查干凹陷中、新生代热史及烃源岩热演化. 地球科学, 38(3): 553-560. doi: 10.3799/dqkx.2013.055
    ZUO Yin-hui, MA Wei-min, DENG Yi-xun, HAO Qing-qing, LI Xin-jun, GUO Jun-mei, RAN Qing, WANG Li-rong, 2013. Mesozoic and Cenozoic Thermal History and Source Rock Thermal Evolution History in the Chagan Sag, Inner Mongolia. Earth Science, 38(3): 553-560. doi: 10.3799/dqkx.2013.055
    Citation: ZUO Yin-hui, MA Wei-min, DENG Yi-xun, HAO Qing-qing, LI Xin-jun, GUO Jun-mei, RAN Qing, WANG Li-rong, 2013. Mesozoic and Cenozoic Thermal History and Source Rock Thermal Evolution History in the Chagan Sag, Inner Mongolia. Earth Science, 38(3): 553-560. doi: 10.3799/dqkx.2013.055

    查干凹陷中、新生代热史及烃源岩热演化

    doi: 10.3799/dqkx.2013.055
    基金项目: 

    国家自然科学基金 91114202

    国家自然科学基金 90914006

    重庆市自然基金重点项目 CSTC2012jjB90007

    详细信息
      作者简介:

      左银辉(1980-), 男, 博士, 主要从事沉积盆地热体制和地球动力学的研究.E-mail: zuoyinhui@tom.com

    • 中图分类号: P314

    Mesozoic and Cenozoic Thermal History and Source Rock Thermal Evolution History in the Chagan Sag, Inner Mongolia

    • 摘要: 查干凹陷是内蒙古银-额盆地最具勘探潜力的凹陷, 为了揭示查干凹陷中、新生代热史及烃源岩热演化历史, 首先利用9口井的镜质体反射率数据恢复了查干凹陷中、新生代热史, 结果显示查干凹陷在早白垩世巴音戈壁组沉积开始至银根组沉积末期, 地温梯度逐渐增加, 且到银根组沉积末期达到最大, 为50~58 ℃/km; 自晚白垩世乌兰苏海组沉积开始至今, 地温梯度逐渐下降, 现今地温梯度仅为31~34 ℃/km.再以热史为基础, 结合沉积和构造发育史及烃源岩地球化学资料, 模拟了查干凹陷9口井3套烃源岩的成熟度演化历史, 模拟结果显示查干凹陷烃源岩成熟度演化受古地温控制, 3套烃源岩成熟度都在早白垩世晚期达到最大.

       

    • 图  1  查干凹陷构造划分及井位

      Fig.  1.  Structural division and well locations in the Chagan sag

      图  2  查干凹陷镜质体反射率数据与深度的关系(井位见图 1)

      虚线范围内的数据受苏红图组火山活动的影响, 且影响程度不一致, 导致同一深度镜质体反射率相差较大, 不能用于热史模拟

      Fig.  2.  Vitrinite reflectance data versus depth in the Chagan sag

      图  3  力1井埋藏史、热史及生烃史模拟结果

      Fig.  3.  The modeled results of burial, thermal and hydrocarbon generation history of well Li 1

      图  4  查干凹陷典型井热演化历史

      Fig.  4.  Thermal evolution history of typical wells in the Chagan sag

      图  5  中央构造带典型井烃源岩成熟度演化历史

      Fig.  5.  Maturation history of typical wells in the central tectonic zone

      图  6  乌力吉断鼻构造带典型井烃源系成熟度演化历史

      Fig.  6.  Maturation history of typical wells in the Wuliji fault-nose tectonic zone

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    • 收稿日期:  2012-02-02
    • 刊出日期:  2013-05-15

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