| 福建福鼎会甲溪地热带特征及其成矿模式 |
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| 引用本文： | 戴清忠,陈荣魁,张晓东.福建福鼎会甲溪地热带特征及其成矿模式[J].福建地质,2002,21(3):137-143. |
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| 作者姓名： | 戴清忠 陈荣魁 张晓东 |
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| 作者单位： | 福建省第四地质大队,宁德,352100 |
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| 摘 要： | 福鼎会甲溪地热带属断裂构造深循环型中低温地热，位于南溪三角隆起断块上，受控制于北西向会甲溪断裂，温泉（井）出露于北西向构造与近东西向，北北东向构造交汇处。在总结地热带特征的基础上，建立成矿模式，评价地热资源及找矿远景。
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| 关 键 词： | 福建 地热 成矿模式 找矿远景 地层 岩浆岩 |
| 修稿时间： | 2001年10月23 |
Characteristics of the Hujiaxi Thermal Belt and Its Ore-forming Pattern, in Fuding, Fujian Province |
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| Dai qingzhong,Chen Rongkui,Zhang Xiaodong.Characteristics of the Hujiaxi Thermal Belt and Its Ore-forming Pattern, in Fuding, Fujian Province[J].Geology of Fujian,2002,21(3):137-143. |
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| Authors: | Dai qingzhong Chen Rongkui Zhang Xiaodong |
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| Abstract: | The Huijiaxi thermal belt in Fuding, Fujian Province, located at the Nanxi triangle upwraping, belongs to the tectonic and deep circulating geotherm of low-to-moderate temperature and is controlled by the Huijiaxi northwest-trend fault. The thermal springs(wells) are scattered in the interjunction between the northwest-trend structures and near east-west and north-northeast-trend structures. Based on the analysis results of the characteristics of the thermal belt, in the paper the authors made a pattern of forming the thermal belt and put forward a way to evaluate the geothermal resources of the surveyed area. |
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| Keywords: | characteristics of thermal belts ore-forming pattern ore-finding target Fuding Fujian Province |
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