| 注册
首页|期刊导航|高校地质学报|初论华南加里东花岗岩与大规模成矿作用的关系

初论华南加里东花岗岩与大规模成矿作用的关系

华仁民 张文兰 陈培荣 翟伟 李光来

高校地质学报Issue(1):1-11,11.
高校地质学报Issue(1):1-11,11.

初论华南加里东花岗岩与大规模成矿作用的关系

Relationship Between Caledonian Granitoids and Large-scale Mineralization in South China

华仁民 1张文兰 1陈培荣 1翟伟 2李光来1

作者信息

  • 1. 内生金属矿床成矿机制研究国家重点实验室南京大学,南京210093
  • 2. 中山大学 海洋学院,广州 510275
  • 折叠

摘要

Abstract

The Caledonian granites take the second importance among the multi-aged granitoids in so-called South China Large Granite Province. However, the pervious studies show less concern on the metallogenic aspects of Caledonian granites. Some early studies considered no important mineralization related to Caledonian granites. Based on some newly discovered granitic intrusions of Caledonian ages, together with the synthetic assessment of related literature, the present paper reviews the general character of Caledonian granites and discusses the relationship between Caledonian granites and large scale rare metal metallogeneses in South China. Although the large-scale rare metal mineralization mainly took place in the Yanshanian Period of Late Jurassic Era, Caledonian granitoids of mostly Silurian Era made great positive effects. Some well-evolved Caledonian granites, such as those in Penggongmiao of southeastern Hunan, Niutangjie of northern Guangxi, Guiling of northeastern Guangxi, and Qingjie of Youjiang area, can cause W, Mo and Sn mineralization. Some others might serve as rare metal supply for mineralization associated with late-staged granites, such as Shilei of southern Jiangxi and Meiziwo of northern Guangdong. At Yijiang of southern Hunan, the weathering products of Caledonian quartz diorite form a unique REE-Sc deposit. The most important significance, however, is that the Caledonian Orogeny started the intra-continental crust evolution of South China. The Caledonian granitoids resulted mainly by melting of crust materials, instead of adding of mantle material. The following tectonic episodes such as Variscan, Indo-sinian, and Yanshanian, together with the accompanying granitic magmatism, promoted the forward evolution of crust. As a result, the crust of South China became highly matured, which is indicated by high enrichment of felsic components and lithophile rare metals, and finally yielded the largest rare metal mineralization in the world.

关键词

加里东期/花岗岩/大规模成矿/华南

Key words

Caledonian/granite/large-scale mineralization/South China

分类

天文与地球科学

引用本文复制引用

华仁民,张文兰,陈培荣,翟伟,李光来..初论华南加里东花岗岩与大规模成矿作用的关系[J].高校地质学报,2013,(1):1-11,11.

基金项目

国家自然科学基金项目(41073035,41230315) (41073035,41230315)

国家重点基础研究发展计划(2007CB411404)资助 (2007CB411404)

高校地质学报

OA北大核心CSCDCSTPCD

1006-7493

访问量0
|
下载量0
段落导航相关论文