羌塘盆地泉水化学特征及其意义
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国家自然科学基金项目(编号: 40473001)和中国地质调查局“我国陆域永久冻土带天然气水合物资源远景调查”项目(编号: 200410100001)联合资助。


Chemic charactoristics of fountains in Qiangtang Basin Qinghai-Tibet Plateau and its implications
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    摘要:

    水文地球化学在石油、天然气找矿方面应用十分广泛,而且取得了较好的效果,天然气水合物与常规油气有相似的物源和地表化探异常形成机制,因此我们在对青藏高原羌塘盆地的天然气水合物相关的异常进行调查研究时,对取自羌塘盆地的19个泉水样品进行了化学组分、氢氧同位素、水溶甲烷和碳同位素进行了测试分析。研究认为,按照苏林的分类原则羌塘盆地泉水主要为Na2SO4型和NaHCO3型;泉水的矿化度,显示以低矿化度的淡水、微淡水为主;氢氧同位素分析表明泉水来源以大气降水为主;泉水中均检测到一定含量的水溶甲烷,水溶甲烷碳同位素分析表明泉水为油田相关地下水。综合分析认为本次研究所采集的羌塘盆地泉水主要来自大气降水;各采样点泉水中均检测出一定含量的水溶气甲烷,通过对水溶甲烷含量较高样点泉水的δ13C的分析认为泉水不同程度的受地下油气藏影响。综合分析后认为,SQ-2、SQ-17可大致指示地下油气藏或天然气水合物藏的具体位置。

    Abstract:

    While water chemistry is widely used in oil & natural gas exploration and make good effect, we chosed it in gas hydrate which has similarity with oil & natural gas in origin & surface chemical abnormity exploration in Qiangtang Basin Qinghai-Tibet Plateau. We achieved 19 fountain samples in Qiangtang Basin, and had it tested it in National Gas-geochemisty Key Laboratory Lanzhou Institute of Geology Chinese Academy of Sciencences. According to the test result we recognize that the 19 fountains are mainly fresh or low mineralized water, typed as Na2SO4 & NaHCO3 according to Sulin’s water sorting principle. Hydrogen & Oxygen isotope analysis indicate the mainly rainfall origin of the fountains. Dissolved methane and its carbon isotope 13C test show that it may come from oil or gas hydrate buried deep in the ground. In conclusion that SQ-2 & SQ-17 may point out the possible position of oil & gas or natural gas hydrate deposit.

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张志攀,祝有海,苏新.2011.羌塘盆地泉水化学特征及其意义[J].地质学报,85(7):1233-1238.
zhangzhipan, zhuyouhai, suxin.2011. Chemic charactoristics of fountains in Qiangtang Basin Qinghai-Tibet Plateau and its implications[J]. Acta Geologica Sinica,85(7):1233-1238.

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  • 收稿日期:2009-01-19
  • 最后修改日期:2009-03-26
  • 录用日期:2009-07-02
  • 在线发布日期: 2011-07-18
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