摘要
为进一步研究罗次温泉的地热成因,本文在充分收集区域及前人资料基础上,采用测量、调查、取样分析等手段,结合已有钻探资料、同位素分析及观测资料,从热源、热储、盖层、通道等方面对该区地热地质条件进行总结,建立热储模型,从岩性条件、构造条件、热源条件等方面分析总结了温泉成因特征,认为罗次温泉主要受罗次—易门断裂控制,热储结构呈条带状,为典型的断裂带型小型地热田.研究结果为罗次温泉的合理开发利用提供了详实依据,同时也为今后该地区的地热地质研究工作提供了参考.
Abstract
In order to further study the geothermal genesis of Luoci Hot Spring,this paper summarizes the geothermal geological conditions of the area from the aspects of heat source,heat storage,cover layer,and chan-nel,based on sufficient collection of regional and previous materials,and using methods such as measurement,survey,and sampling analysis.Combined with existing drilling data,isotope analysis,and observation data,a thermal storage model was established.The study summarized the genetic characteristics of Luoci Hot Spring from lithological conditions,structural conditions,and heat source conditions.It is believed that Luoci Hot Spring is mainly controlled by the Luozi-Yimen Fault,and the thermal storage structure is layered,forming a typical small-scale geothermal field of the fault zone type.The research results provide a detailed basis for the rational develop-ment and utilization of Luoci Hot Spring,and also provide a reference for the geothermal geological research in the area in the future.
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