中文摘要:依据地热流体成矿作用基本要素的特殊性、成矿控制因素及其控矿特点，对地壳演化运动的成矿控制及其规律性等方而进行了较系统的分析。研究结果表明，地热流体是特殊的热液成矿作用类型，与其它成矿作用类型有明显的区别。
Abstract:Based on the particularity of essential factors of geothermal fluid mineralization, factors controlling the ore-forming process, and ore-control characteristics, the present paper has systematically analysed the relationship between metallogenesis and crustal evolution process. It is known from the analysis that the geothermal fluid mineralization is a special type of hydrothermal ore-forming process obviously distinguishable from other mineralization types.
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基金项目:湖南省自然科学基金项目“湖南中西部锑矿床成矿机理、成矿规律及找矿方向的研究”专题（94-12）
引用文本：
张术根.1998.地热流体成矿作用分析[J].矿床地质,17(1):91~96.1998.An analysis of geothermal fluid mineralization[J].Mineral Deposits17(1):91~96
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