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现代地质 ›› 2015, Vol. 29 ›› Issue (5): 1164-1172.

• 天然气水合物调查评价专辑 • 上一篇    下一篇

青海木里三露天天然气水合物矿藏土壤微量元素地球化学特征

孙忠军1,杨志斌1,卢振权2,张富贵1,张舜尧1,周亚龙1,王惠艳1   

  1. (1.中国地质科学院 地球物理地球化学勘查研究所,河北 廊坊065000; 2.中国地质调查局 油气资源调查中心,北京100029)
  • 出版日期:2015-10-29 发布日期:2015-12-24
  • 作者简介:孙忠军,男,研究员,1961年出生,地球化学专业,主要从事油气和天然气水合物研究与勘查。 Email:sunzhongjun@igge.cn。
  • 基金资助:

    国土资源部公益性行业专项(201111019);国土资源部天然气水合物专项(GZHL20110324, GZH201400302)。

Geochemical Characteristics of Trace Elements in Soil above Sanlutian Natural Gas Hydrates in the Qilian Mountains

SUN Zhong-jun1, YANG Zhi-bin1, LU Zhen-quan2, ZHANG Fu-gui1, ZHANG Shun-yao1, ZHOU Ya-long1, WANG Hui-yan1   

  1. (1.Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, Hebei065000, China;
    2.Oil & Gas Survey, China Geological Survey, Beijing100029, China)
  • Online:2015-10-29 Published:2015-12-24

摘要:

在祁连山冻土区木里天然气水合物矿区进行了微量元素地球化学勘查有效性试验,试验面积150 km2,采样密度2个点/km2。研究表明,土壤Ba、V、Fe 、Ca等元素在水合物矿藏上方呈现顶部异常,而且异常吻合程度较高。微量元素预测天然气水合物具有较高的成功率,调查前钻探的干井(DK-4、DK-5和DK-6)位于背景区,调查前钻探的水合物井(DK-1、DK-2、DK-3、DK-7)和调查后水合物井(DK3-11、DK2-13、DK1-14)位于异常内。试验结果还预测了祁连山天然气水合物两个新的远景区。试验表明,微量元素是祁连山冻土区寻找天然气水合物的有效指示元素,它们与水合物其它化探指标结合冻土条件和地质特征综合解释,可以提高冻土区天然气水合物预测成功率。

关键词: 祁连山冻土区, 天然气水合物, 微量元素, 顶部模式, 地气迁移机理

Abstract:

The efficiency test of trace element geochemical exploration was carried out for natural gas hydrates in the Qilian Mountains permafrost region, the study area covered 150 km2 and sampling density of 2 sampling sites per km2 was used. Results showed that Ba, V, Fe and Ca in soils presented the apical pattern, and had identical anomalies. Natural gas hydrates could be higher successfully prospected by trace elements. The dry wells ( DK-4, DK-5, DK-6)drilled before this survey were located in background area, and the hydrate wells DK-1, DK-2, DK-3, DK-7 drilled before the survey and DK3-11, DK2-13, DK1-14 drilled after the survey were both located in anomaly area. Two prospective target regions were predicted according to the test results. Test has shown that trace elements were the effective index for prospecting gas hydrate in the Qilan Mountain permafrost region. Combined with permafrost conditions and geological characteristics, the comprehensive interpretation of trace elements and other geochemical index could improve the success rate of prediction for natural gas hydrate in permafrost area.

Key words: Qilian Mountains permafrost, gas hydrate, trace element, apical pattern, mechanism of geogasmigration

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