摘要
据多种类型铀矿区域地质规律,总结出判别未知区铀成矿远景模式,分析康滇地轴地壳演化历史中的铀成矿作用,认为晋宁运动前没有铀成矿作用,澄江期、海西期、印支-燕山期,分别有一次铀成矿作用。其中可能澄江期的铀成矿作用较为重要。
In this paper, according to the regional metaltogenetic regularity of various types of the uranium deposits, the recognition of the uranium metallogenetic prospective model in an unknown area is summarized and uranium mineralization in the evolutional process of the earth's crust of the Xikang-Yunnan Axis is analysed. The author points out that uranium mineralization had not developed before the Jinning Movement, but it was developed during Chengjiang period, Hereynian period and Indochina-Yanshanian period, respectively, among them, uranium mineralization during Chengjiang period was much more important,
出处
《铀矿地质》
CSCD
北大核心
1992年第6期348-353,378,共7页
Uranium Geology
