摘要
桂东-汝城钨锡多金属成矿区是南岭有色、稀有金属成矿带的重要组成部分。近年来,该区找矿工作取得了明显进展,新发现了竹园里、上山、大岭背等一批具大型找矿前景的钨锡多金属矿产地,矿床类型多样。本文通过对区内成矿地质条件及矿床地质特征的研究,探讨了矿床成因,并分析了找矿前景,提出了找矿方向。
The Guidong-Rucheng tungsten-tin polymetallic metallogenic region is an important part of Nanling nonferrous and rare metal metallogenic province.A set of deposits,such as Zhuyuanli,Shangshan and Dalingbei,are newly found which indicates a great prospecting potential in this area.Based on study of regional metallogenetic conditions and geological characteristics of those deposits,genesis of the ore-fields are in-depth discussed,and the further prospecting direction is provided by our theoretical and practical works.
出处
《华南地质与矿产》
CAS
2010年第2期8-14,共7页
Geology and Mineral Resources of South China
基金
国土资源大调查资源评价项目(1212010781074)
关键词
钨锡多金属矿床
燕山期花岗岩
矿床成因
找矿前景
桂东-汝城地区
tungsten-tin polymetallic deposits
Yanshanian granite
genesis of deposit
prospecting potential
Guidong-Rucheng area
