地质找矿论丛2017，Vol.32Issue(4)：562-569,8.DOI:10.6053/j.issn.1001-1412.2017.04.006
四川省康定县赫德钨锡矿地质特征及矿床成因
Geological characteristics and genesis of Hede tungsten-tin depositin Kangding county, Sichuan province
摘要
Abstract
Hede tungsten-tin polymetallic deposit is a greisen-quartz vein type deposit occurring at the northern end of the Lanniba excessive granite body.This paper analyzes the geological characteristics and genesis of the ore deposits and suggests that the mineralization is controlled by multi-factors (strata,structure,magmatic rock) and overprinting of the factors.The ore materials mainly come from the sial crust.The ore is formed at post-magma pneumatogenic hydrothermal fluid stage during Late indosinian period (210.0 Ma-213 Ma).关键词
钨锡矿床/地质特征/矿床成因/赫德地区/四川省Key words
tungsten-tin deposit/geological characteristics/genesis of deposit/Hede/Sichuan分类
天文与地球科学引用本文复制引用
杨涛,辛存林,安国堡..四川省康定县赫德钨锡矿地质特征及矿床成因[J].地质找矿论丛,2017,32(4):562-569,8.基金项目
“四川省康定县赫德矿区钨锡矿补充勘查”项目. （）
