摘要
应用区域构造成矿分析和成矿系列理论,在分析研究区域地质构造、银矿床成因及时空分布规律的基础上,划分了湘南银矿床成因类型,指出湘南地区存在与花岗岩类有关的岩浆热液矿床( )、与一定地质时期和地层单位有关的层控矿床( )和与表生成矿作用有关的风化淋滤矿床( )三大类银矿床;其中 类型银矿床占主导地位, 类型银矿床仅在局部产出, 类型银矿暂不具工业意义。同时,圈出了东坡-许家山、坪宝、铜山岭-后江桥3个找矿远景区。
Based on study of regional geological background,genesis and distribution regulation,silver deposits in Southern Hunan Province are divided into magmatichydrothermal type(Ⅰ) related to granitoids,stratacontrolled type(Ⅱ),weatheringinfiltration type(Ⅲ),among which the magmatichydrothermal type is the most important,stratacontrolled type is controlled by some special strata and weatheringinfiltration type currently shows no industrial significance.Three prospecting regions for silver deposits in the studied area are also suggested,including the DongpoXujiashan,Huangshapingbaoshan and TongshanlingHoujiangqiao area.
出处
《华南地质与矿产》
CAS
2003年第3期43-48,共6页
Geology and Mineral Resources of South China
基金
中国白银地质基金委员会"南岭银矿"研究项目.
关键词
银矿
找矿方向
湘南地区
区域构造
成矿分析
type of silver deposit
prospecting region
southern Hunan Province