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西藏山南地区明则斑岩钼矿床蚀变矿化特征与成矿时代
引用本文:范新.西藏山南地区明则斑岩钼矿床蚀变矿化特征与成矿时代[J].地质与勘探,2011,47(1):89-99.
作者姓名:范新
作者单位:中国科学院地质与地球物理研究所矿产资源研究重点实验室;中国科学院研究生院;中国冶金地质总局第二地质勘查院;中国冶金地质总局;
基金项目:中国冶金地质总局“冈底斯东段南部矽卡岩-斑岩Cu-Au-Mo矿床成矿条件及成矿模式综合研究”; 国家自然科学基金项目(编号:40772066)资助
摘    要:明则斑岩钼矿床位于冈底斯成矿带的东南缘,雅鲁藏布江缝合带北侧.矿区内主要出露有钾长花岗岩、黑云母二长花岗岩、花岗闪长岩、似斑状二长花岗岩及花岗斑岩,其中花岗斑岩为成矿岩体.围岩蚀变较为强烈,主要的蚀变特征有:钾化、硅化、绿泥石化、高岭土化和矽卡岩化,而且各种蚀变现象具有垂向分带特征,其中矽卡岩化主要发育在地表浅部,岩体...

关 键 词:蚀变矿化特征  明则斑岩Cu(Mo)矿40Ar-39Ar年代学  成矿时代  冈底斯南缘
收稿时间:2010/10/12 0:00:00
修稿时间:2010/11/26 0:00:00

Characteristics of Alteration and Mineralization and Chronology of the Mingze Porphyry Mo Deposit in the Shannan Area of Southern Tibet
FAN Xin.Characteristics of Alteration and Mineralization and Chronology of the Mingze Porphyry Mo Deposit in the Shannan Area of Southern Tibet[J].Geology and Prospecting,2011,47(1):89-99.
Authors:FAN Xin
Institution:FAN Xin1,2,CHEN Lei1,QIN Ke-zhang1,XIAO Bo1,LI Jin-xiang1,LI Qiu-ping3,CHEN Yu-shui3,CHEN Jin-biao3,ZHAO Jun-xin1,LI Guang-ming1,HUANG Shu-feng3,JU Yi-tai4(1.Key Laboratory of Mineral resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,2.Graduate University of Chinese Academy of Science,Beijing 100049,3.No.2 Institute of China Metallurgical Geology Bureau,Putian 351111,4.Institute of Mineral Resources Research,China Metallurgical Geology Bureau,Beijing 100025)
Abstract:The Mingze porphyry Mo deposit is located in the southeastern margin of the Gandese metallogenic belt,north of the Yarlung Zangbo River suture zone.A variety of intrusions outcrop such as moyite,biotite monzogranite,granodiorite,porphyaceous adamellite and granite porphyry.The granite porphyry is the ore-froming related intrusion which is completely mineralized.Wall rocks suffered extensive alteration,mainly as potassic,silicification,chloritization,kaolinization and skarn alteration.Various types of altera...
Keywords:40Ar-39Ar chronology  metallogenic epoch  mineralization characteristics  Mingze porphyry Mo(Cu)deposit  southern Gandese  
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