南海神狐海域非均质性天然气水合物储层的分频反演

吴淑玉, 徐华宁, 刘俊, 杨睿, 宁伏龙. 南海神狐海域非均质性天然气水合物储层的分频反演[J]. 海洋地质与第四纪地质, 2020, 40(6): 106-120. doi: 10.16562/j.cnki.0256-1492.2020031901
引用本文: 吴淑玉, 徐华宁, 刘俊, 杨睿, 宁伏龙. 南海神狐海域非均质性天然气水合物储层的分频反演[J]. 海洋地质与第四纪地质, 2020, 40(6): 106-120. doi: 10.16562/j.cnki.0256-1492.2020031901
WU Shuyu, XU Huaning, LIU Jun, YANG Rui, NING Fulong. Frequency-divided inversion method of heterogenous natural gas hydrates reservoir in the Shenhu area, South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 106-120. doi: 10.16562/j.cnki.0256-1492.2020031901
Citation: WU Shuyu, XU Huaning, LIU Jun, YANG Rui, NING Fulong. Frequency-divided inversion method of heterogenous natural gas hydrates reservoir in the Shenhu area, South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 106-120. doi: 10.16562/j.cnki.0256-1492.2020031901

南海神狐海域非均质性天然气水合物储层的分频反演

  • 基金项目: 国家重点研发计划“天然气水合物储层高精度刻画技术”(2017YFC0307406);国家海洋局海底重点实验室基金“台西南盆地沉积基底特征和莫霍面构造形态综合地球物理研究”(KLSG1603)
详细信息
    作者简介: 吴淑玉(1985—),女,在读博士,副研究员,主要从事地震资料解释和反演工作,E-mail:hnwushuyu@163.com
    通讯作者: 徐华宁(1973—),男,博士,教授级高工,主要从事天然气水合物成像与反演等综合研究,E-mail:xuhuaning1973@163.com
  • 中图分类号: P738

Frequency-divided inversion method of heterogenous natural gas hydrates reservoir in the Shenhu area, South China Sea

More Information
  • 南海北部陆坡神狐海域天然气水合物钻探结果显示,这一区域水合物储层具有纵横向分布不均质性、规模小且变化快的特点,使得精确评价水合物资源量面临诸多困难。根据井震数据分析了水合物分布特点,利用分频反演方法对该区水合物的空间分布进行预测。分频反演是利用测井和地震资料,采用支持向量机(SVM)的方法研究不同探测频率下的振幅响应(AVF),将AVF作为独立信息引入反演,建立起测井和地震波形间的非线性关系,充分利用地震中全频带信息,实现高分辨率的反演结果。采用该方法进行预测的结果与实际钻井情况非常吻合,验证这一技术适用于预测非均质性天然气水合物空间分布。基于预测结果并结合区域地质特征综合分析表明:水合物分布不均匀的主控因素除温压条件外,晚中新世之后的频繁构造运动使较深部的热解气沿着断层、气烟囱向上运移,形成厚块状“流体运移通道型”天然气水合物藏,而浅部沉积物中以扩散方式在渗透性良好的储层形成薄层状天然气水合物藏。

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  • 图 1  楔状模型的频率—厚度—振幅响应

    Figure 1. 

    图 2  南海北部大陆边缘珠江口盆地区域构造与研究区位置图[61]

    Figure 2. 

    图 3  BSR在地震剖面上的反射特征

    Figure 3. 

    图 4  含水合物沉积层W03井的测井曲线

    Figure 4. 

    图 5  楔状模型正演下不同反演方法储层厚度识别对比

    Figure 5. 

    图 6  声波阻抗和电阻率的交会图

    Figure 6. 

    图 7  水合物地震剖面的频谱特征

    Figure 7. 

    图 8  井旁道分频地震属性SVM训练结果与电阻率测井曲线对比

    Figure 8. 

    图 9  原始和90°相位剖面与井曲线对比

    Figure 9. 

    图 10  分频反演剖面与W03井深探测电阻率曲线

    Figure 10. 

    图 11  神狐海域水合物成藏分布模式图

    Figure 11. 

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出版历程
收稿日期:  2020-03-19
修回日期:  2020-07-09
刊出日期:  2020-12-25

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