摘要
华南赣杭构造带是典型的火山岩型铀矿床成矿带,其铀矿成矿时代、控矿规律及热液蚀变等方面有一定的共同特征。铀成矿流体主要为深源高温、高压、中高盐度、富含挥发分的还原性流体,晚期有大气降水加入,富铀基底和富集地幔可能共同提供了成矿物质,成矿期铀可能主要以正四价杂化配合物形式运移。矿床的形成是中生代大陆热点作用晚期的产物。
The Gan-Hang tectonic belt is a typical volcanic-type uranium mineralization belt. There arecertain extent common features in mineralization ages, ore-controlled characteristics, mineral association and hydrothermal alteration for the uranium deposits in this region. The min-eralization fluids are chartered by high temperature, high pressure, middle-high salinity, volatile-bearing and deoxidize and influxing of circulated meteoric water in later stage. The ore-forming mattersare sourced fromuranium-enriched basement and enriched mantle, and the uranium was mainlymigrated astheuranous hybrid complexes in metallogenic stage. The formation of uranium deposits is closely associated with Mesozoic continental hot spots.
出处
《西北地质》
CAS
CSCD
2017年第1期25-34,共10页
Northwestern Geology
基金
中核集团“龙灿工程”相山基础地质研究项目(LCD116)
关键词
赣杭构造带
火山岩型铀矿
成矿规律
大陆热点作用
成矿模式
Gan-Hang tectonic belt
volcanic-type uranium
common features in mineralization
continental hot spots
metallogenic model