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额尔古纳超大型火山热液型铀成矿带地质特征及找矿前景
引用本文:罗毅,王正邦.额尔古纳超大型火山热液型铀成矿带地质特征及找矿前景[J].华东地质学院学报,1997,20(1):1-10.
作者姓名:罗毅  王正邦
作者单位:核工业北京地质研究院
摘    要:本文介绍了在额尔古纳超大型火山热液型铀成矿带中发现的超大型火山热液脉型铀矿末有5个,大型火山热液脉型铀矿床有6个,总共有铀金属储量33万t,在世界热液脉型铀矿资源量中占有重要地位。经研究认为,该成矿带内铀矿就成矿作用在时间上具有突发性特征,成矿时代集中在早白垩世,受统一中生代大陆裂陷-火山岩浆活动控制;成矿介质中深源的火山岩水,大气水和变质水三者相混合的具中低温的火山热液,成矿物质主要来自中生代深

关 键 词:铀矿床  成矿带  地质特征  找矿前景  火山热液

The Geologic Characteristics and Prospecting Prospect of Eerguna Super large volcanic Hydrothermal Type Uranium Metallogenic Belt
Luo\,Yi\ \ Wang Zhengbang\ \ Zhou Dean.The Geologic Characteristics and Prospecting Prospect of Eerguna Super large volcanic Hydrothermal Type Uranium Metallogenic Belt[J].Journal of East China Geological Institute,1997,20(1):1-10.
Authors:Luo\  Yi\ \ Wang Zhengbang\ \ Zhou Dean
Abstract:This belt has 5 super large volcanic hydrothermal vein type uranium deposits and 6 large size volcanic hydrothermal vein type uranium deposits with a total reserve of 330 000 t and holds an important position in the hydrothermal vein type uranium resources of the world.The study shows that the metallogenesis of the uranium deposits in this metallogenic belt has features of abruptness on time.The metallogenic epoches are concentrated in early Cretaceous,and uranium metallization are controlled by a united Mesozoic continental taphrogenic volcano magmatic activity.The metallogenic media are moderate low temperature volcanic hydrothermal solutions originated from the mixing of deep volcano magmatic water,meteroric water and metamorphic water.The ore forming materials are mainly derived from Mesozoic deep enrichment type magmatic source.
Keywords:Super large uranium deposit  metallogenic geologic features  prospecting prospect    
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