逊克县宝山铜钨钼矿床地质特征及成因

J4 ›› 2008, Vol. 16 ›› Issue (2): 46-47.

逊克县宝山铜钨钼矿床地质特征及成因

高若峰，荆龙华，魏连喜

黑龙江省有色金属地质勘查研究总院，黑龙江哈尔滨 150042

收稿日期:2007-12-05 修回日期:2008-02-23 出版日期:2008-04-27 发布日期:2011-07-04
作者简介:高若峰(1969一)，男，_丁程帅，主要从事地质勘查工作

Geological Features and Genesis of Gold Deposit in Copper，Tungsten and Molubdenum Baoshan Xunke Canton

GAO Ruofeng，JING Longhua，WEI Lianxi

Heilongjiang Central Academy of Nonferrous Mental Geology Eexploration and Research，Harbin 150046，Heilongjiang，China

Received:2007-12-05 Revised:2008-02-23 Online:2008-04-27 Published:2011-07-04

摘要/Abstract

摘要：

通过对逊克县宝山铜钨钼多金属矿床的野外调查和室内工作，对矿床地质特征及控矿条件的特征分析，从铜钨钼矿与断裂、岩体、围岩蚀变的关系特征揭示了铜钨钼矿的地质特征，探讨了矿床成因和找矿标志，对今后该区带的找矿工作具指导意义。

关键词: 铜钨钼矿床, 地质特征, 矿床成因, 逊克县宝山

Abstract:

From the field investigation and indoor work of Baoshan Xunke county ，this paper studied copper，tungsten and m0lybdenum polymetallic deposit，by the analysis of geological characteristic and ore—controlling condition of songping gold deposit，the relationship between copper，tungsten，molybdenum and fracture，rock—body and wallr0ck alteIlati0n I℃vea1ed the geological characteristics about copper，tungsten and molybdenum． By studying the cause of dep0sit and prospecting mark，it will have an direction significance in ore prospecting in this area·

Key words: \Molybdenum, Copper and tungsten ore—forming, Geologic characteristics, Ore—form ing cause baoshan xunke canton

中图分类号:

P618．65

高若峰，荆龙华，魏连喜. 逊克县宝山铜钨钼矿床地质特征及成因[J]. J4, 2008, 16(2): 46-47.

GAO Ruofeng，JING Longhua，WEI Lianxi. Geological Features and Genesis of Gold Deposit in Copper，Tungsten and Molubdenum Baoshan Xunke Canton[J]. J4, 2008, 16(2): 46-47.

参考文献

[1] 曲关生，浦全生，韩松山，等．黑龙江省岩石地层[M]．北京：中国地质大学出版社，1997．
[2] 韩振新，许衍强，郑庆道．黑龙江省重要金属和非金属矿产的成矿系列及其演化[M]．哈尔滨：黑龙江人民出版社，2004．
[3] 云富，周庆仁，罗玉兴，等．区域地质调查报告(逊克县等幅)[R]．哈尔滨：黑龙江省地质局，1981．
[4] 金艳峰，张传乐，寇秀峰．延边中西部地区钼矿成矿地质特征[J]．吉林地质，2004，23(3)：53—57．
[5] 陈国达．成矿构造方法[M]．北京：地质出版社，1995．

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed