内蒙古达茂旗查干哈达庙铜多金属矿床地质特征

胡格吉乐吐; 姜大伟; 杨丹妮

doi:10.13686/j.cnki.dzyzy.2013.06.003

内蒙古达茂旗查干哈达庙铜多金属矿床地质特征

1.
内蒙古地质勘查有限责任公司, 内蒙古呼和浩特 010020;

2.
内蒙古自治区地质矿产勘查开发局, 内蒙古呼和浩特 010020

详细信息

作者简介: 胡格吉乐吐(1983-),男(蒙古族),从事地质勘查工作,通信地址内蒙古呼和浩特市呼伦南路161号,E-mail//49720761@qq.com

中图分类号: P618.41

收稿日期: 2012-11-05

修回日期: 2013-01-04

刊出日期: 2013-12-31

GEOLOGICAL CHARACTERISTICS OF THE CHAGANHADAMIAO COPPER POLYMETALLIC DEPOSIT IN INNER MONGOLIA

1.
Inner Mongolia Geological Exploration Co., Ltd., Hohhot 010020, China;

2.
Inner Mongolia Bureau of Geological Exploration and Development, Hohhot 010020, China

Received Date: 05 November 2012

Revised Date: 04 January 2013

Publish Date: 31 December 2013

摘要

摘要: 内蒙古查干哈达庙铜矿床位于内蒙-兴安造山带西段之华力西晚期褶皱带内，哲斯敖包复向斜南翼，受北东-北北东向断裂构造及下二叠统大石寨组变质岩系控制.该矿区矿化体赋存于下二叠统大石寨组三岩段（P1d3）的英安质凝灰岩、凝灰岩中，严格受北东向断裂构造控制.铜矿体为含铜石英脉体，赋存于北东向断裂构造中.矿区内共圈定7个铜矿体，矿体总体走向为北东-北北东向，倾角43~75°.铜矿体呈脉状、透镜状，有分支现象，厚度变化小，属稳定型.通过系统总结矿床的矿体地质、矿物成分、矿物嵌布及围岩蚀变特征，认为铜矿成矿与变质岩系、断裂构造、岩浆热液活动有关，矿床成因类型为岩浆热液型.
- 地质特征 /
- 成矿条件 /
- 岩浆热液 /
- 矿床成因 /
- 查干哈达庙铜矿床 /
- 内蒙古
Abstract: The Chaganhadamiao copper deposit in Inner Mongolia, located on the south wing of Zhesiaobao synclinorium in the Late Variscan fold belt of western Inner Mongolia-Xingan orogenic belt, is controlled by the NE-NNE-trending faults and Lower Permian Dashizhai metamorphic formation. The orebodies, occurring as Cu-bearing quartz veins, are hosted in the dacitic tuff of the third member of Lower Permian Dashizai Formation. The deposit consists of 7 copper orebodies, which generally trend to NE-NNE, with dip angles between 43° and 75°. With study on the geology of deposit, mineral composition, mineral occurrence and wallrock alteration, it is suggested that the copper mineralization should be related to the metamorphic rocks, faults and magmatic hydrothermal activities. The deposit belongs to magmatic hydrothermal type in genesis.
- geological characteristics /
- metallogenic condition /
- magmatic hydrothermal fluid /
- genesis of deposit /
- Chaganhadamiao copper deposit /
- Inner Mongolia

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内蒙古达茂旗查干哈达庙铜多金属矿床地质特征

1. 内蒙古地质勘查有限责任公司, 内蒙古 呼和浩特 010020; 2. 内蒙古自治区地质矿产勘查开发局, 内蒙古 呼和浩特 010020

作者简介: 胡格吉乐吐(1983-),男(蒙古族),从事地质勘查工作,通信地址 内蒙古呼和浩特市呼伦南路161号,E-mail//49720761@qq.com

GEOLOGICAL CHARACTERISTICS OF THE CHAGANHADAMIAO COPPER POLYMETALLIC DEPOSIT IN INNER MONGOLIA

1. Inner Mongolia Geological Exploration Co., Ltd., Hohhot 010020, China; 2. Inner Mongolia Bureau of Geological Exploration and Development, Hohhot 010020, China

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1.
内蒙古地质勘查有限责任公司, 内蒙古呼和浩特 010020;

2.
内蒙古自治区地质矿产勘查开发局, 内蒙古呼和浩特 010020

作者简介: 胡格吉乐吐(1983-),男(蒙古族),从事地质勘查工作,通信地址内蒙古呼和浩特市呼伦南路161号,E-mail//49720761@qq.com

1.
Inner Mongolia Geological Exploration Co., Ltd., Hohhot 010020, China;

2.
Inner Mongolia Bureau of Geological Exploration and Development, Hohhot 010020, China