Transactions of Nonferrous Metals Society of China The Chinese Journal of Nonferrous Metals

您目前所在的位置:首页 - 期刊简介 - 详细页面

中国有色金属学报

ZHONGGUO YOUSEJINSHU XUEBAO

第27卷    第9期    总第222期    2017年9月

[PDF全文下载]        

    

文章编号:1004-0609(2017)-09-1916-13
湘东大垄铅锌矿床成矿机理
邵拥军1, 2,隗含涛1, 2,郑明泓1, 3,刘忠法1, 2,熊伊曲1, 2,徐卓彬1, 2,蒋梦同1, 2

(1. 中南大学 有色金属成矿预测与地质环境监测教育部重点实验室,长沙 410083; 2. 中南大学 地球科学与信息物理学院,长沙 410083; 3. 贵州省有色金属和核工业地质勘查局,贵阳 550005)

摘 要: 大垄铅锌矿床位于湘东新华夏构造体系中坊楼北北东向构造带中部南东侧,邓阜仙复式岩体北端,矿体受南北向断裂控制。通过电子探针、流体包裹体和S、Pb、H、O同位素研究,分析矿床的成矿物质来源、成矿物理化学条件,探讨矿床成因及成矿过程。结果表明:矿床的形成与燕山期岩浆活动密切相关,成矿物质具有壳幔混合的特征,成矿流体主要源于岩浆水,有大气降水的加入;成矿温度属于中低温,成矿初期流体处于弱碱性、弱氧化的环境,后期向低温、低氧逸度、低硫逸度的环境转换,成矿深度为中深成。综合认为大垄铅锌矿床属于与燕山期岩浆活动有关的中低温热液铅锌矿床。

 

关键字: 电子探针;流体包裹体;同位素;成矿机理;大垄铅锌矿床

Mineralization mechanism of Dalong Pb-Zn deposit, eastern Hunan Province, China
SHAO Yong-jun1, 2, WEI Han-tao1, 2, ZHENG Ming-hong1, 3, LIU Zhong-fa1, 2, XIONG Yi-qu1, 2, XU Zhuo-bin1, 2, JIANG Meng-tong1, 2

1. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Central South University, Changsha 410083, China; 2. School of Geoscience and Info-Physics, Central South University, Changsha 410083, China; 3. Non-Ferrous Metals and Nuclear Industry Geological Exploration Bureau of Guizhou, Guiyang 550005, China

Abstract:Dalong Pb-Zn deposit is located in the southeast of the middle Fanglou NNE structural belt of Neocathaysian structural system and the north head of the Dengfuxian composite granite. Ore occurrence is controlled by south-north faults. Through the electron microprobe analysis, fluid inclusions and S, Pb, H, O isotope characteristics research, the source of ore-forming materials, ore-forming physicochemical conditions were analyzed, and the ore deposit genesis and metallogenic process were discussed. The results indicate that the formation of ore bodies is closely related to the Yanshanian magmatic activity; the ore-forming materials have the feature of crust-mantle mixing; the ore-forming fluid is mainly derived from magmatic water, but with the mixing of atmospheric precipitation; the metallogenetic temperature is low-medium temperature; the ore-forming fluid is weak alkali, weak oxidizing environment, and late it transforms to low temperature and low oxygen fugacity of low sulfur fugacity environment; the metallogenetic depth is shallow-moderate depth. Dalong Pb-Zn deposit belongs to low-medium temperature magmatic hydrothermal deposit relating to the Yanshanian magmatic activity.

 

Key words: electronic mircoprobe? fluid inclusion? isotope? metallogenic mechanism? Dalong Pb-Zn deposit

ISSN 1004-0609
CN 43-1238/TG
CODEN: ZYJXFK

ISSN 1003-6326
CN 43-1239/TG
CODEN: TNMCEW

主管:中国科学技术协会 主办:中国有色金属学会 承办:中南大学
湘ICP备09001153号 版权所有:《中国有色金属学报》编辑部
------------------------------------------------------------------------------------------
地 址:湖南省长沙市岳麓山中南大学内 邮编:410083
电 话:0731-88876765,88877197,88830410   传真:0731-88877197   电子邮箱:f_ysxb@163.com