摘要
对前人深源热液金属元素(包括铀)和铀成矿文献的综述可以得出:地幔流体-重大地质事件-成矿构造是深源铀成矿靶区勘查模式。探讨了南岭铀成矿带的成矿潜景和深层勘查方法,提示构造地球化学、金属活动态提取技术作为该区深源找铀矿方法所起的重要作用。
This paper is a review on metal elements(including uranium)metallogenesis of deep-source hydrothermal fluids. It is discovered that mantle fluid-major geological event and ore-forming structure compose the metallogenetic and prospecting model for deep-source uranium deposit. Metallogenetic potentials and exploration methods for Nanling metallogenetic belt are discussed. It is pointed out that structural geochemistry and extraction techniques of metal mobile forms have played an important role as the methods to discover deep-source uranium deposits in Southest China.
出处
《世界核地质科学》
CAS
2007年第2期63-67,共5页
World Nuclear Geoscience
关键词
地幔流体
重大地质事件
表壳控矿构造
南岭铀成矿带
mantle fluids
great geological event
crustal ore-controlling structure
Nanlinguranium metallogenetic belt