大兴安岭南段铜多金属矿构造控矿特征分析

现代地质 ›› 2007, Vol. 21 ›› Issue (Suppl): 30-34.

大兴安岭南段铜多金属矿构造控矿特征分析

徐毅，张寿庭，王长明，刘晓吉

中国地质大学地球科学与资源学院,北京100083

收稿日期:2006-11-01 修回日期:2006-12-07 出版日期:2007-08-20 发布日期:2007-08-20
作者简介:徐毅，男，博士研究生，1980年出生，矿产普查与勘探专业，主要从事矿田构造研究。
基金资助:
中国地质大学地质过程与矿产资源国家重点实验室基金项目；内蒙古地矿重大科技项目（内地研2004-05）

Analysis on Structure Control Characteristics of Cu-polymetallic Deposits in the Southern Section of the Da Hinggan Mountains, Inner Mongolia

XU Yi, ZHANG Shou-ting, WANG Chang-ming, LIU Xiao-ji

School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China

Received:2006-11-01 Revised:2006-12-07 Online:2007-08-20 Published:2007-08-20

摘要/Abstract

摘要：

大兴安岭南段地区为我国重要铜多金属成矿带，矿床（点）的产出和分布特征严格受构造控制，褶皱和断裂为区内主要控矿构造形迹。NE向区域深大断裂带为研究区的主体控岩控矿构造，与旁侧NNE、NW、EW向次级断裂构成复杂的网格状构造系统，矿床（点）主要分布于断裂结点处，表现出较强的分带性和递变性特征，构造复合控矿特征明显。研究区矿体、矿脉多呈不规则脉状、复脉状、透镜状产出，沿断裂带膨缩变化断续延伸。不同方向控矿断裂的交叉与分支复合部位，以及同一断裂的产状变化地段是找矿有利地段。

关键词: 大兴安岭南段, 铜多金属矿, 控矿构造

Abstract:

Lying in Inner Mongolia, the southern section of the Da Hinggan Mountains is one of the most important polymetallic belts in China. In this region, mineral deposits are obviously controlled by structures which are mainly folds and fractures. The basic pattern of structures is in NE direction. Mineral deposits (points) are dominantly distributed in the intersections of NE, NNE, NW and EW fractures. They display strongly zoning and gradually changing. The ore bodies disconnectedly distribute along the fractures as irregular veins or lens. The preferable ore-finding areas are the intersections of different directions fractures or the sections of faults where the attitude changed.

Key words: the southern section of , the Da Hinggan Mountains, Cu-polymetallic deposits, ore-controlled structure

中图分类号:

P613
P618.4

徐毅，张寿庭，王长明，刘晓吉. 大兴安岭南段铜多金属矿构造控矿特征分析[J]. 现代地质, 2007, 21(Suppl): 30-34.

XU Yi, ZHANG Shou-ting, WANG Chang-ming, LIU Xiao-ji. Analysis on Structure Control Characteristics of Cu-polymetallic Deposits in the Southern Section of the Da Hinggan Mountains, Inner Mongolia[J]. Geoscience, 2007, 21(Suppl): 30-34.

[1]	张梅, 翟裕生, 沈存利, 刘永慧, 杨帅师, 翟德高, 要梅娟, 王建平, 王守光, 高征西, 张玲. 大兴安岭中南段铜多金属矿床成矿系统[J]. 现代地质, 2011, 25(5): 819-831.
[2]	王瑾, 侯青叶, 陈岳龙, 刘金宝, 王忠, 冷福荣. 内蒙古维拉斯托铜多金属矿床流体包裹体研究[J]. 现代地质, 2010, 24(5): 847-855.
[3]	康明. 岑况. 罗先熔. 陈祥.. 内蒙古东部闹牛山—巨里河铜多金属矿带岩浆活动与成矿的关系[J]. 现代地质, 2004, 18(2): 210-216.