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甲玛铜多金属矿床锆石微量元素基本特征及成因意义
引用本文:胡志莲,汪雄武,秦志鹏,张俊成,高一鸣,彭惠娟. 甲玛铜多金属矿床锆石微量元素基本特征及成因意义[J]. 有色金属(矿山部分), 2012, 64(5): 58-63
作者姓名:胡志莲  汪雄武  秦志鹏  张俊成  高一鸣  彭惠娟
作者单位:1. 成都理工大学地球科学学院,成都,610059
2. 中国地质科学院矿产资源研究所,北京,100037
基金项目:中央公益性行业科研专项"西藏甲玛斑岩铜多金属矿科学基地研究"
摘    要:甲玛铜多金属矿四个斑岩岩体中锆石阴极发光形态显示多数为岩浆锆石,少数为热液锆石和继承锆石核。稀土配分型式均呈现重稀土元素相对富集而轻稀土元素相对亏损,少数配分型式分散且轻稀土元素含量较高的为热液锆石。Ti、Ce、(Sm/La)N、Nb/Hf等元素含量及比值范围均位于岩浆区域。所研究的锆石主要为岩浆成因,但受到热液流体作用影响。锆石特征可为判断同类型斑岩矿床的成矿潜力提供理论依据,并指导找矿。

关 键 词:岩浆锆石  热液锆石  继承锆石核  指导找矿

Basic characteristics of zircon trace elements and their genetic significances in Jiama Copper Polymetallic Deposit
HU Zhilian , WANG Xiongwu , QIN Zhipeng , ZHANG Juncheng , GAO Yiming , PENG Huijuan. Basic characteristics of zircon trace elements and their genetic significances in Jiama Copper Polymetallic Deposit[J]. , 2012, 64(5): 58-63
Authors:HU Zhilian    WANG Xiongwu    QIN Zhipeng    ZHANG Juncheng    GAO Yiming    PENG Huijuan
Affiliation:1.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China; 2.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China)
Abstract:Zircon Cathode Luminescence images of the four major porphyry plutons in Jiama Copper Polymetallic Deposit show that most of them are magmatic origin,and few of them are hydrothermal(altered) zircons and inherited cores.They are characterized by enrichment of HREE and depletion of LREE.A few zircon grains have high LREE contents and diverse REE patterns,which might have been resulted from hydrothermal alteration.Both Ti & Ce contents and(Sm/La)N & Nb/Hf ratios fall in the domain of magmatic zircons.Most zircons from four porphyry plutons in Jiama Deposit are magmatic origin,but a few of them were altered by hydrothermal fluids.The characteristic of zircon can provide theory basis for judging the same type porphyry deposit metallogenic potential,and which can also guide the ore-prospecting work.
Keywords:magmatic zircon  hydrothermal(altered) zircon  inherited zircon core  guidance for ore exploration
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