摘要
锑矿床研究的重点包括 :锑矿床分类 ;不同构造环境下锑矿床的成因模式 ;锑的来源。今后锑矿床分类将以锑矿床形成的构造背景为主 ,结合锑矿床成因方式和容矿主岩特点来进行。文章介绍了几种典型构造环境下 (大型走滑、造山挤压和造山崩坍 )锑矿床形成机理和成因模式。现有的资料表明锑矿床受壳幔相互作用所制约 (如拆沉作用 ,delamination) 。
The most important problems in the study of antimony deposits include classification of antimony deposits, genetic models of antimony deposits in various tectonic settings, and antimony sources. In further classification of antimony deposits, we should consider tectonic settings, origin of antimony deposits and host rocks. This paper deals with genetic models of antimony deposits in different tectonic settings. The data of antimony deposits indicate that the formation of antimony deposits is controlled by such interactions between the crust and the mantle as delamination. This seems to be the most important and difficult problem.
出处
《矿床地质》
CAS
CSCD
北大核心
2000年第2期166-172,共7页
Mineral Deposits
基金
国土资源部资助!定向课题(编号 :98-14)和973课题 (编号 :G1999043206)
关键词
锑矿分类
构造环境
拆沉作用
深部来源
锑矿床
classification of antimony deposits, tectonic setting, delamination, deep source
