摘要
根据近年来作者的研究成果，就目前人们对花岗岩型铀矿床成因的几种认识进行了评述。在此基础上，讨论了∑ＣＯ＿２对铀成矿的制约和地壳拉张与铀成矿的关系。针对目前热液矿床研究中存在的问题，提出了加强成矿作用矿化剂地球化学研究的必要性。
In the light of author's work on uranium deposits located in or near S-type granite of SouthChina , this paper has commented upon the former points of view on their geneses, and discussed therelation among ∑CO_2,the crustal extension and uranium metallogeny.Direct towards the problemsin former genetic research on hydrothermal ore deposits, the paper finally suggests that it is necessaryto make efforts to strenthen the study of mineralizer geochemistry of mineralization.
出处
《地球科学进展》
CAS
CSCD
1994年第2期41-46,共6页
Advances in Earth Science
基金
国家自然科学基金
关键词
铀矿床
矿床成因论
花岗岩型
Granite-type uranium deposits, Deposit origin, Earth crust extension,∑CO_2, Min-eralizer.
