摘要
千里山-骑田岭矿集区是南岭成矿带的重要组成部分,位于华夏、扬子两大内陆板块碰撞拼贴带与郴州-邵阳走滑型构造岩浆岩带的交汇部位。通过对区内主要金属矿床的研究,认为区内矿床的形成及其矿物组合与一定的时代和特定的大地构造环境紧密相关,不同的大地构造环境下所形成的矿床,其成因类型有明显的差异;不同成因类型的矿床,有各自特有的矿物组合。
The Qianlishan-Qitianling mineralized concentration area,located in the convergent area of the Yangtze and Cathaysian plate and in the Chenzhou-Shaoyang strike-slip tectonomagmatic zone,is an important part of the Nanling metallogenic belt in the region.On the basis of study on main deposits,the authors recognize that the forming of deposits and their mineral assemblages show close relation with particular tectonic settings and geological ages:the genetic types of mineral deposits formed in various tectonic settings are different and different types of mineral deposits have different mineral assemblages.
出处
《华南地质与矿产》
CAS
2003年第4期51-55,共5页
Geology and Mineral Resources of South China
基金
中国地质调查局"中国主要成矿区带研究"的子课题研究项目(K1.4-2-14).
关键词
大地构造环境
矿物组合
千里山-骑田岭矿集区
板块碰撞
tectonic setting
mineral asemblages
Qianlishan-Qitianling mineralized concentration area
