摘要
黄岗梁-乌兰浩特锡铅锌铜多金属成矿带,地处内蒙古东南部,近北东走向,长约400km,是铜、铅、锌、锡、银等多金属矿产的集中分布区。本文在综合前人研究的基础上,对研究区的区域成矿地质背景、成矿时空特征、成矿条件与成矿机制进行了探讨,总结出3个矿床成矿系列9个矿床式。
Huanggangliang-Wulanhaote tin-lead-zinc-copper-polymetallic metallogenic belt is located in the southeastern part of Inner Mongolia.Near the North East direction,about 400km,is the copper,lead,zinc,tin,silver and other metal mineral concentration distribution.In this paper,a comprehensive basis of previous studies,the study area on the regional metallogenic geological setting,ore-forming space-time characteristics of ore-forming conditions and ore-forming mechanisms are discussed,summed up the three metallogenic series and 9-style deposit.
出处
《中国矿业》
北大核心
2010年第6期100-104,共5页
China Mining Magazine
基金
中央级公益性科研院所基本科研业务费项目(编号:K0921)
关键词
成矿带
时空架构
成矿机制
黄岗梁
乌兰浩特
metallogenic belt
space-time structure
ore-forming mechanism
Huanggangliang
Wulanhaote
