铀矿地质2016，Vol.32Issue(6)：357-362,6.DOI:10.3969/j.issn.1000-0658.2016.06.005
修水姜坑地区碳硅泥岩型铀矿成矿特征及找矿方向
The Metallogenic Conditions and Prospecting Direction Analysis of Carbonate-Siliceous-Argillitic Type Uranium Ore Deposits in Jiangkeng,Xiushui
王阳平 1彭波1
作者信息
- 1. 江西省核工业地质局 267 大队，江西 九江 332000
- 折叠
摘要
Abstract
Jiangkeng area is located in intersection parts Xuefeng-Jiurui and Xiushui-Ningguo-Kaihua car-bonate-siliceous-argillitic type uranium metallogenic belt namely,xiushui Dongkeng-Donggang syncline in Jiurui polymetallic metallogenic belt.One small and medium-sized uranium deposits have been discov-ered in this syncline.The exploration area have similar lithofacies paleogeographic environment,struc-ture,lithology and other ore-forming geological characteristics which show good prospecting potential. In this paper, ore-prospecting work in recent years was summarized and analogy predecessors information was analysed, it was considered that the mineralization in this area is mainly of hydrothermal superimposed transformation which was jiontly controlled by the Zhoushantuo formation of Sinian and the interlayer fracture zone there is still a great potential for the exploration of the red beds in the northwest of the work area.关键词
碳硅泥岩型铀矿/修水地区/找矿方向Key words
carbonate-siliceous-argillitic type uranium deposits/Xiushui area/prospecting direction分类
天文与地球科学引用本文复制引用
王阳平,彭波..修水姜坑地区碳硅泥岩型铀矿成矿特征及找矿方向[J].铀矿地质,2016,32(6):357-362,6.
