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| 西藏绒多矽卡岩型铜多金属矿床地质特征及找矿标志 | |
| 引用本文： | 周辉,莫洪智,周普红,李红明.西藏绒多矽卡岩型铜多金属矿床地质特征及找矿标志[J].矿产与地质,2010,24(3):217-221. |
| 作者姓名： | 周辉 莫洪智 周普红 李红明 |
| 作者单位： | 1. 桂林理工大学,广西,桂林,541004 2. 中国冶金地质总局中南地质勘查院,武汉,430081 3. 中国地质大学,北京,100083 |
| 基金项目： | 致谢：笔者在野外和室内工作中得到中南地质勘查院王泽华、谢德全、余中明、彭强国、刘雁群、章奋兵等高工的帮助和指导,在撰写过程中桂林矿产地质研究院黄永平教授级高工、桂林工学院胡云沪教授提出了很多宝贵建议,在此一并致谢! |
| 摘 要： | 冈底斯成矿带是一条重要的铜多金属成矿带,绒多铜多金属矿床位于冈底斯成矿带东段,矿床类型为与燕山晚期岩浆活动密切相关的矽卡岩型。文章通过对矿区地层、构造、岩浆岩、矿体及矿石的特征进行研究,总结了矿床地质特征和成矿规律,并对控矿因素和矿床成因进行了探讨,对今后矿区及其外围的找矿工作具指导意义。 |
| 关 键 词： | 铜多金属矿床 矽卡岩型 地质特征 找矿标志 冈底斯东段 |
Geological characteristics and prospecting criteria of Rongduo sharn copper polymetallic deposit in Tibet |
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| ZHOU Hui,MO Hong-zhi,ZHOU Pu-hong,LI Hong-ming.Geological characteristics and prospecting criteria of Rongduo sharn copper polymetallic deposit in Tibet[J].Mineral Resources and Geology,2010,24(3):217-221. | |
| Authors: | ZHOU Hui MO Hong-zhi ZHOU Pu-hong LI Hong-ming |
| Institution: | 1.Guilin University of Technology,Guilin,Guangxi 541004;2.Central South Institute of Geological Exploration,China General Bureau of Metallurgy Geology,Wuhan,Hubei 430081;3.China University of Geosciences,Beijing 100083) |
| Abstract: | Gangdese metallogenic belt is an important copper polymetallic belt.Rongduo copper polymetallic deposit is located in eastern Gangdese,which are the skarn-type copper polymetallic deposits with closely related to late Yanshanian age magmatic activity.By studying the ore field stratum,tectonics,magmatic rocks,orebody and ore characteristics,it has summarized geological characteristics and metallogenic regularity of the deposit and discussed ore-controlling factors and origin of ore deposit.It has guiding significance for the mining area and its peripheral prospecting in the future. |
| Keywords: | sharn deposits copper polymetallic deposit eastern Gangdese geological characteristics prospecting criteria |
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