摘要
用现代成矿理论,结合水文地质学和地热学,对广西区内的地热水成矿特征研究发现,广西的地热水矿床在区域上的分布受深部构造的隆起区(带)和区域深大断裂控制,决定地热水矿床空间定位的主要因素是沉积盆地、断裂、褶皱、岩浆岩、地貌、盖层与热储层。划分出广西区内三种地热水储层及四种地热水成矿类型,初步建立了成矿模式,指出了区内地热水矿床的四大找矿远景区。
Research on the characteristics of geothermal water in Guangxi shows the distribution of geothermal water occurrence is controlled by deep structure upwarping regions (zone) and by the regional deep fracture.The main factors which control the location of geothermal water deposits location are faults, folds, magmatic rock, land form, cap rock and geothermal water reservoir. In the article, three types of geothermal water reservoir, four types of geothermal water deposit and four types of potential provinces for prospecting are divided.
出处
《矿产与地质》
2004年第2期103-108,共6页
Mineral Resources and Geology
关键词
地热水
找矿方向
控矿因素
类型
Hydrothermal water
prospecting direction
controlling factor
type
