海螺沟温泉地质成因分析
Genetic analysis of Hailuogou hotspring
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摘要: 通过泉域地质构造、水文地质条件的分析,根据温泉的水文地球化学特征,从温泉的水源、热源、构造等方面阐明了海螺沟温泉的成因,认为海螺沟温泉是接受充沛大气降水、冰雪融水、河水补给的岩溶裂隙、构造裂隙水向下作深部循环,在不同深度汇入海螺沟断裂破碎带及影响带,与来自深部地壳的呈"蒸汽蒸馏"状的高温高压热流产生混合作用,同时进行热交换、离子交换、溶滤、吸附等热物理、化学作用,生成了泉域特定水化学特征的高温热矿水,并在适宜的构造、地貌部位溢出,形成的热泉。对海螺沟地区地热资源的开发利用和旅游地质的研究具有一定的参考价值。Abstract: This paper expounds the origin of Hailuogou hotspring in water source,heat source and structure through analyzing the regional geology,hydrogeologic conditions and hydrogeochemical features.The hotspring is recharged by karst and tectonic fissure water which derives from precipitation,meltwater and river water,which flows and cycles deep down to Hailuogou fracture zone and affected zone where the water and "steam distillation" from deep crust with high temperature and pressure are mixed,and at the meantime,some related physical and chemical processes such as heat exchange,ion exchange,lixiviation and adsorption are proceeded.All these factors generate the high temperature mineral water with unique hydrochemical characteristics.The hotspring is found where the tectonic structure and landform are suitable.It has the great value to exploit the geothermal resources and study the geological tourism in Hailuogou.
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