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越城岭-猫儿山地区花岗岩特征及成矿
引用本文:冯国玉,黄杰,何方.越城岭-猫儿山地区花岗岩特征及成矿[J].矿产与地质,2009,23(5):412-417.
作者姓名:冯国玉  黄杰  何方
作者单位:桂林矿产地质研究院,广西,桂林,541004
基金项目:广西有色金属集团有限公司地质找矿科研项目(GYDK09001)《越城岭-猫儿山花岗岩体钨锡钼矿找矿预测研究》资助 
摘    要:越城岭-猫儿山地区花岗岩类岩石出露很广,侵入时代从加里东期至燕山期,为一套富硅、铝过饱和、燕山早期花岗岩体略富碱、分异演化程度较高的中粒-细粒黑云母花岗岩、二云母花岗岩和白云母花岗岩。岩石具有明显的富K2O,贫Na2O特征,为富含W、Sn、Pb和Bi的岩体,具备了为钨锡多金属矿化提供成矿物质和成矿热流体的内在条件。区内钨锡钼矿化与燕山早期花岗关系密切,矿床(点)产于细粒花岗岩周边、细粒花岗岩体与围岩接触带附近。

关 键 词:花岗岩  成矿  越城岭-猫儿山

The features and metallogenesis of the granites in the Yuechengling-Maoershan area
FENG Guo-yu,HUANG Jie,HE Fang.The features and metallogenesis of the granites in the Yuechengling-Maoershan area[J].Mineral Resources and Geology,2009,23(5):412-417.
Authors:FENG Guo-yu  HUANG Jie  HE Fang
Institution:FENG Guo-yu,HUANG Jie,HE Fang(Guilin Research Institute of Geology for Mineral Resources,Guilin,Guangxi 541004)
Abstract:The Granites are extensively exposed in the Yuechengling-Miaoershan region,ranging in age from Caledonian to Yanshannian.This suit is comprised of middle-fine-grained biotite-granites,fine-grained muscovite-biotite-granites and fine-grained muscovite-granites which are rich in silica,alkalis,aluminum,high evolution and high differentiation.The granites are K2O rich and Na2O poor and W-Sn-Pb-Bi-rich rocks.W-Sn-Mo metallogenesis is correlated to early Yanshannian granites in the area.The majority of deposits ...
Keywords:tin-polymetallic deposit  granite  metallogenesis  Yuechengling-Maoershan  
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