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。
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.
出处
《福建地质》
2002年第3期137-143,共7页
Geology of Fujian
关键词
福建
地热
成矿模式
找矿远景
地层
岩浆岩
characteristics of thermal belts, ore-forming pattern, ore-finding target, Fuding, Fujian Province
