南极半岛别林斯高晋海天然气水合物成矿条件与成矿机理

何韵, 杨木壮. 南极半岛别林斯高晋海天然气水合物成矿条件与成矿机理[J]. 海洋地质前沿, 2018, 34(4): 16-24. doi: 10.16028/j.1009-2722.2018.04003
引用本文: 何韵, 杨木壮. 南极半岛别林斯高晋海天然气水合物成矿条件与成矿机理[J]. 海洋地质前沿, 2018, 34(4): 16-24. doi: 10.16028/j.1009-2722.2018.04003
Yun HE, Muzhuang YANG. FORMING CONDITIONS AND MECHANISM OF GAS HYDRATES IN THE BELLINSGAUZEN SEA, ANTARCTIC PENINSULA[J]. Marine Geology Frontiers, 2018, 34(4): 16-24. doi: 10.16028/j.1009-2722.2018.04003
Citation: Yun HE, Muzhuang YANG. FORMING CONDITIONS AND MECHANISM OF GAS HYDRATES IN THE BELLINSGAUZEN SEA, ANTARCTIC PENINSULA[J]. Marine Geology Frontiers, 2018, 34(4): 16-24. doi: 10.16028/j.1009-2722.2018.04003

南极半岛别林斯高晋海天然气水合物成矿条件与成矿机理

  • 基金项目:
    国家专项专题(DD20160214-01);教育部人文社科规划课题(14YJA630083)
详细信息
    作者简介: 何韵(1994-),女,在读硕士,主要从事国土资源规划利用研究.E-mail:heyunho@163.com
  • 中图分类号: P744.4

FORMING CONDITIONS AND MECHANISM OF GAS HYDRATES IN THE BELLINSGAUZEN SEA, ANTARCTIC PENINSULA

  • 位于南极半岛西侧的别林斯高晋海是南极附近海域天然气水合物成矿的远景区域。利用现有钻孔岩心样品、地震剖面、声波等资料,从气源、稳定域、构造输导及沉积储集等方面,分析了别林斯高晋海天然气水合物的形成条件,预测了天然气水合物成矿远景区,初步探讨了其形成机理,以期能为今后南极半岛区域的天然气水合物资源调查研究提供一定的科学参考依据。
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  • 图 1  别林斯高晋海区位、主要构造及钻孔位置示意图

    Figure 1. 

    图 2  ODP 178航次1096钻孔沉积物地球化学指标的垂向变化特征(据文献[20])

    Figure 2. 

    图 3  天然气水合物的温-压条件分析图(据文献[4, 22]修改)

    Figure 3. 

    图 4  南极陆缘热流分布图(紫色圆点为热流数据站位;据文献[23])

    Figure 4. 

    图 5  多道地震剖面识别的南极半岛西侧陆缘BSR(据文献[26])

    Figure 5. 

    图 6  别林斯高晋海盆地沉积物总体分布(据文献[31, 33])

    Figure 6. 

    图 7  别林斯高晋海海底自然地理状况图(据文献[10])

    Figure 7. 

    图 8  天然气水合物成矿主要区域及形成机制

    Figure 8. 

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收稿日期:  2018-02-10

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