资源调查与环境Issue(3)：211-217,7.
华南花岗岩型铀矿地质特征及成矿作用
Geological characteristics and mineralization of the granite-type uranium deposits in south China
邵飞 1许健俊 1邵上 2姚鹏飞 1刘琨 1吴闻涛 1张莹1
作者信息
- 1. 核工业270研究所，江西南昌330200
- 2. 核工业290研究所，广东韶关512026
- 折叠
摘要
Abstract
Basing on systematizing the predecessors’ achievements in prospecting and research on gran-ite-type uranium resources in our country for more than fifty years ,and applying research means such as geochemistry and induction of objective geological phenomena ,the geological characteristics of the granite- <br> type uranium deposits in south China are summarized as follows :The uranium-producing intrusions belong to composite massifs , the uranium-producing granites possess characteristics of intracontinental S-type granites ,large time differences are shown between mineralization and diagenesis ;ore-forming is obviously controlled by geological interfaces .Basing on understanding the dynamics processes of “source ,transpor-tation and aggregation”in the uranium mineralization ,focusing on the source of ore-forming materials and the evolution of ore-fluid system ,the granite-type uranium mineralization in south China is explained .It is believed that the source of ore-forming materials was originated from the regional Late Sinian and Early Cambiran uranium source beds ,the invasion of vein rock after large-scale magmatic activities prompted the regional fluids to locally evolve to ore-forming fluids ,which were driven by gravity and buoyancy and were transported by faults acting as important migration channels ,and the change of physical-chemical condi-tions of the fluids caused the precipitation of ore-forming materials .关键词
花岗岩型铀矿/地质特征/成矿流体演化/成矿作用/华南Key words
granite-type uranium deposit/geological characteristics/evolution of ore-forming fluids/mineralization/South China分类
天文与地球科学引用本文复制引用
邵飞,许健俊,邵上,姚鹏飞,刘琨,吴闻涛,张莹..华南花岗岩型铀矿地质特征及成矿作用[J].资源调查与环境,2014,(3):211-217,7.
