摘要
本文着重论述了上庄坪铜铅锌多金属矿床的地质特征和成矿淀化,进行了成因分析。认为含矿岩系的物源主要来自海底火山喷发作用形成的黄铁矿化矿源层。经燕山期构造热液的叠加,驱使矿源层中的成矿元素活化、迁移,在有利的构造部位富集成矿。
This paper emphasizes the geological characteristics and discuss on the origin analysis of poly-metallic ore deposit in Shangzhuangping. According to the study of the mineral evolving, origin analysis etc., it is considered that the source of minerals etc mainly comes from the pyritization sources of the submarine volcano eruption. By the time of Yanshanian structural hydrothermal superimposed caused the ore - forming chemical dement of the pyritization sources activated, it results from the dements had been moving and expected turning into minerals in the beneficial structural position.
出处
《华南地质与矿产》
CAS
2007年第2期14-18,共5页
Geology and Mineral Resources of South China
关键词
地质特征
成矿演化
成因分析
黄铁矿化
矿源层
Geology characteristic
the mineral evolving
origin analysis
pyritization
the mineral sources.
