西安地裂缝近期活动与热水井水位关系研究
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摘要
本文根据西安小寨地裂缝与西影井第三系深层热水水位的观测资料,分析了二者变化周期的准同步和相位的滞后性特征,并结合地面沉降速率和周围地震活动性,探讨了地裂缝与第三系深层承压水位之间存在内在联系的原因,以及抽水—地面沉降对地裂缝影响的构造动态调制作用.
Based on observition data of Xiaozhai ground fissure and Xiying well's water level, the characteristics of quasi -synchroneity and relationship to phase are analyzed. Combining with the data of ground subsidence rate and seismic activity nearby, we have studied the cause of interrelation between ground fissure and Tertiary deep water, and the effect of water - pumping ground subsidence on the ground fissure.
引文
[1]张家明,等.西安地裂缝研究.西安:西北大学出版社,1990.
    [2]李永善,等.西安地裂及谓河盆地活断层研究.北京:地震出版社,1992.
    [3]景北科.西影深井水位变化与临潼—长安断裂活动.内陆地震,1993.
    [4]刘快胜,等.用地下水资料探讨陕西及周边地震形势.灾害学,1995.

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