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赣南樟东坑钨矿成矿花岗岩及矿化特征

黄小娥 李光来 郭家松 张敏 胡志国 华仁民 韦星林

地质与勘探2012,Vol.48Issue(4):685-692,8.
地质与勘探2012,Vol.48Issue(4):685-692,8.

赣南樟东坑钨矿成矿花岗岩及矿化特征

Characteristics of Ore-forming Granite and Its Mineralization in the Zhangdongkeng Tungsten Deposit of Southern Jiangxi Province

黄小娥 1李光来 2郭家松 1张敏 1胡志国 1华仁民 3韦星林1

作者信息

  • 1. 江西有色地质勘查局,江西南昌330001
  • 2. 南京大学,江苏南京210093 东华理工大学,江西抚州344000
  • 3. 南京大学,江苏南京210093
  • 折叠

摘要

Abstract

The Zhangdongkeng tungsten deposit is a typical quartz vein type tungsten-molybdenum deposit hosted outside the granitic contact zone in the Chongyi-Dayu-Shangyou area.The concealed granites in the mine are dominated by two lithofacies,the main granitic body and the flamboyance vein body.Both of them are ore-forming mother rocks with osculation related to the tungsten-molybdenum mineralization.The granites in the mine district are rich in silicon and aluminum,but poor in iron and magnesium,middling in calcium;more alkali and rich in kalium.The DI index is relatively high,and the ACNK value is more than one.They belong to acidic to utra-acidic and alkalescence to calcium alkalescence rock series,with a high degree of differentiation,near to exceed aluminous,i.e.a kind of remelting-reforming granite type from crust rock.And their geochemical characteristics are rich in Rb,Th,U,K,Ta,and Y trace elements but poor in Ba,Nb,Sr,P,and Ti.The total amount of rare-earth elements is low but relatively rich in light rare-earth ones,and severely depleted in Eu with a "seagull type" of rare-earth element distribution curve.All these indicate further that they are crust type of granites with a high degree of magma evolution.The tungsten-molybdenum mineralization in the mine district is divided into two kinds of type:one is quartz-vine and the other is rock-body,both of them being of mineralizing characters of "upper tungsten-lower molybdenum" and "upper vein-lower body",controlled by intrusion and differential evolution of the granite.The flamboyance granule granitic vein type of tungsten-molybdenum mineralization in Zhangdongkeng is a newly discovered type of mineralization in the vein tungsten mine districts of Chong-Yu-You,southern Jiangxi in recent years,with a good ore-search prospect.

关键词

“上脉下体”/“上钨下钼”/花岗岩演化/岩体型矿化/樟东坑钨矿/赣南

Key words

upper vein-lower body/upper tungsten-lower molybdenum/granite evolution/rock body type of mineralization/Zhangdongkeng tungsten deposit/southern Jiangxi

分类

天文与地球科学

引用本文复制引用

黄小娥,李光来,郭家松,张敏,胡志国,华仁民,韦星林..赣南樟东坑钨矿成矿花岗岩及矿化特征[J].地质与勘探,2012,48(4):685-692,8.

基金项目

国家重点基础研究发展计划 ()

国家自然科学基金项目(41073035)资助的成果 ()

地质与勘探

OA北大核心CSCDCSTPCD

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