文章摘要
贾大成,胡瑞忠,李东阳,卢焱.湘东南地幔柱对大规模成矿的控矿作用[J].地质与勘探,2004,(2):32-35
湘东南地幔柱对大规模成矿的控矿作用
ORE -CONTROLLING ACTIVITY OF THE MANTLE PLUME FOR THE LARGE METALLOGENIC CENTRALIZED REGION IN SOUTHEASTERN HUNAN PROVINCE, CHINA
  修订日期:2002-07-08
DOI:
中文关键词: 地幔柱  控矿作用  大型矿化集中区  湘东南
英文关键词: mantle plume, ore-controlling activity, larger metallogenic centralized region, southeastern Hunan Province
基金项目:国家自然科学基金,中国科学院知识创新工程项目,中国科学院矿床地球化学开放研究实验室基金
贾大成  胡瑞忠  李东阳  卢焱
[1]吉林大学地球探测科学与技术学院,长春130062 [2]中国科学院地球化学研究所矿床地球化学开放研究实验室,贵阳550002 [3]吉林省地质调查院,长春130061
摘要点击次数: 3441
全文下载次数: 1974
中文摘要:
      湘东南是钨、锡、锑及铅锌、稀有、稀土矿床的成矿集中区.该区出露的玄武岩、与成矿有关的花岗岩和区域成矿作用是地幔柱构造环境的统一产物.湘东南地幔柱控制矿床与岩体的时空分布、区域成矿分带和成矿岩浆源区.湘东南地幔柱为成矿岩浆的熔融、分异演化和浅部就位提供了有利的热源和构造条件.地幔柱的发展演化阶段是大规模成矿得以保存的重要因素.
英文摘要:
      There is a larger metallogenic centralized region in the southeastern Hunan province. In the region, basalts, granites related with ore deposits, and regional mineralization were the products of mantle plume tectonic setting. The mantle plume controlled the distribution of rocks and ore deposits, regional metallogenic zoning and metallogenic magma source in the southeastern Hunan province. The mantle plume provided benefiting heat source and structure conditions for the deep melting of metallogenic magma, differentiation and shallow emplacement. The development and revolution of the mantle plume is an important factor for ore deposit preserved.
查看全文   查看/发表评论  下载PDF阅读器
关闭