作 者: (陈江);
机构地区: 成都理工大学地球科学学院,四川成都610059
出 处: 《世界有色金属》 2017年第12期167-168,共2页
摘 要: 我国卡林型金矿床主要分布在黔西南地区,黔西南卡林型金矿集区作为滇黔桂"金三角"重要组成部分,贵州烂泥沟卡林型金矿床自发现以来,一直是地质工作者研究的热点,并取得了丰硕的成果。成矿物质来源包括成矿元素及搬运它的介质—成矿流体的来源问题是矿床地球化学研究的基本问题之一。 Card cover type gold deposits in China are mainly distributed in QianXiNa region, QianXiNa card cover type gold mine area as an important part of dianqiangui "golden triangle", since Lan Ni Gou card cover type gold deposits found in guizhou, has been a hotspot of research on geological workers, and achieved fruitful results. The source of metallogenetic material, including metallogenic elements and the medium of carrying it, is one of the basic problems of geochemical research on mineral deposits.