| 新疆地下热水特征及其与地震活动的关系 |
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| 引用本文： | 王道,许秋龙,陈玲,卢静芳.新疆地下热水特征及其与地震活动的关系[J].地震地质,1999,21(1):58. |
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| 作者姓名： | 王道 许秋龙 陈玲 卢静芳 |
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| 作者单位： | 新疆维吾尔自治区地震局乌鲁木齐,830011 |
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| 摘 要： | 新疆地下热水广泛分布于昆仑山、天山和阿尔泰山。温泉和地震活动与大地构造、板块运动有着密切的联系。动态观测资料分析表明，热水温度变化不仅受到地震的作用，而且显示出某些地震前兆信息。分析了地下热水的化学成分、气体组分、微量元素、放射性元素，认为某些热水具有低矿化、高碱性、高氟、高氦等独特性质，有可能是形成于地壳深部或上地幔的深成水
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| 关 键 词： | 温泉 地震活动 新疆 地下热水 |
A STUDY OF UNDERGROUND HOT WATER OF XINJIANG IN RELATION TO EARTHQUAKES |
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| Wang Dao,Xu Qiulong,Chen Lin,Lu Jinfang.A STUDY OF UNDERGROUND HOT WATER OF XINJIANG IN RELATION TO EARTHQUAKES[J].Seismology and Geology,1999,21(1):58. |
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| Authors: | Wang Dao Xu Qiulong Chen Lin Lu Jinfang |
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| Abstract: | Underground hot water occurs widely in the Kunlun, Tianshan and Artai mountains of Xinjiang. Hot spring, seismicity, tectonics and plate movement are closely related to each other. Analyses of the dynamic observational data show that changes of hot water temperature is influnced by earthquakes and indicates precursors to these events. Chemical analyses have been made to the underground hot water. It is suggested that some hot water have the special nature of low mineralization, high alkalinity, high fluorin |
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| Keywords: | Hot spring Seismicity Xinjiang Underground hot water |
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