摘要
本文在简述崇安─长汀古地堑盆地基本特征的基础上,重点论述了与该地堑盆地相关的金银多金属矿床成矿作用特征,建立了裂谷改造-再造型和裂谷沉积变质-热液叠加改造型两种矿床成因类型,阐明了成矿的机制,建立了成矿模式.
Based on clasifying basic characters of Chong an-Changting paleorift valley basin,this paper expounds mineralization characters of gold-silver-polymetal deposits related to the rift valley basin. New deposit genesis types-rifting reform-repeated formation type and refting sedimentary metamorphic-htdrothermal reform type are established.This paper also clarifies the ore-forming mechanism and establishes ore-forming models.
出处
《华东地质学院学报》
1996年第2期124-132,共9页
Journal of East China Geological Institute
基金
地矿部"八五"部门地质找矿科技攻关项目
关键词
地堑贫地
成矿作用
金矿床
银矿床
多金属矿床
Rift valley basin
gold-silver-polymetal
mineralizationcharacters
morthwestern Fujian