中央亚洲活动带多岛海地质演化与砂岩型铀矿时空定位模式  

Archipelagic Geologic Evolution of Central Asia Mobile Belt and the Timespace Localization Model of Sandstone Type Uranium Deposits

作　　者：刘红旭[1,2] 陈祖伊[2] 郭华 王润红 

机构地区：[1]中国地质大学(北京),北京100083 [2]核工业北京地质研究院,中核集团铀资源勘查与评价技术重点实验室,北京100029 [3]中铁资源有限公司,北京100055

出　　处：《铀矿地质》2014年第2期78-86,共9页Uranium Geology

基　　金：中国核工业地质局基础地质研究项目(地D0502)

摘　　要：中央亚洲活动带是世界上重要的铀成矿带之一,我国的天山-阴山-燕山以北地区正处于此带内。文章以成熟陆壳控矿理论和多岛海地质构造演化理论为基础,在系统分析该成矿带不同构造单元古生代岩石地球化学特征及其反映的大地构造属性的基础上,探讨了该带地壳成熟度及其对后期砂岩型铀矿成矿作用的影响,并建立了相应的砂岩型铀矿时空定位模式。The central Asia mobile belt is one of the most important uranium metallogenic belts in the world, areas of China to the north of Tianshan- Yinshan- Yanshan is just located within this uranium metallogenie belts. Based on the ore - controlling theory of mature continental crust and archipelagic geologic - tectonic evolution, this paper systematically analyzed the petrographic and petrogeochemical characteristics of Paleozoie igneous rocks and the tectonic attributes of different tectonic units in the study region, and discussed the Paleozoic crustal maturity and its influence to subsequent sandstone type uranium metallogenesis, and the time - space localization model of sandstone type uranium deposits was set up.

关 键 词：中央亚洲活动带 多岛海地质演化 地壳成熟度 时空定位模式 

分 类 号：P612[天文地球—矿床学]