我国特色成矿系统的研究进展与重点关注的科学问题  

The Scientific Progress and Some Key Scientific Problems of Chinese Special Mineralization System

作　　者：张鸿翔[1] 

机构地区：[1]中国科学院资源环境科学与技术局,北京100864

出　　处：《地球科学进展》2009年第5期563-570,共8页Advances in Earth Science

摘　　要：中国位于全球三大成矿域的交汇部位,成矿条件优越。同时发育有几种独具特色的成矿系统,如西南大面积低温成矿域、峨眉山地幔柱成矿系统以及广泛分布在华北的前寒武纪条带状铁矿,引起国内外地质学界的广泛关注。对这3种特殊的成矿系统近年来的科研进展进行了综述性回顾,并提出今后需要加强研究的若干重要科学问题。China is located on the intersection among three global mineralization settings. Some special mineralization systems were paid more attention, such as Emeishan mantle plume mineralization system, large low-temperature mineralization setting in the southwestern part of China and BIFs. In this paper, the scientific progress about these special mineralization systems was introduced systematically. Meanwhile, some key scientific problems were discussed.

关 键 词：特色成矿系统 低温成矿域 地幔柱成矿 铁矿 

分 类 号：P61[天文地球—矿床学]