CAJ | 학술논문

亚欧东西向活化构造铀成矿带，其铀资源量约为全球的50％，是全球最重要的大陆洲际铀成矿带。该带地质构造和成矿复杂，活化构造作用延续时间最长，从早元古宙至今断续发生活化作用，以中新生代活化最为强烈。文章从大地构造及其演化控矿的角度，以铀成矿域为单元，对划分该铀成矿带的大地构造、深部构造、地球物理、地球化学和铀成矿分布等依据及铀成矿域分布作初步论述。
아구동서향활화구조유성광대，기유자원량약위전구적50％，시전구최중요적대륙주제유성광대。해대지질구조화성광복잡，활화구조작용연속시간최장，종조원고주지금단속발생활화작용，이중신생대활화최위강렬。문장종대지구조급기연화공광적각도，이유성광역위단원，대화분해유성광대적대지구조、심부구조、지구물리、지구화학화유성광분포등의거급유성광역분포작초보논술。
Over half of the global uranium resources occurred along the east-west activated Eurasian tectonic belt which is the most important in the world.The geological structure and uranium mineralization are complicated in the belt.From early Proterozoic ,the tectonic activity occurred intermittently ,Especially in the Mesozoic and Ce-nozoic period , the activity were the most strongest.In this paper , the basis of the geotectology , deep-crustal stracture ,geophysic-geochimistry and distribution of uranium mineralization were discussed for the division of the reactivated tectonic uranium metallogenic belt and the distribution of uranium mineralization provinces from the views of geotectonics and evolution ore controlling.