湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用

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湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用

朱大岗, 孟宪刚, 王建平, 田晓娟, 刘湘勤, 赵建光

文章导航 > 地质力学学报 > 1998 > 4(1): 63-71

朱大岗, 孟宪刚, 王建平, 等, 1998. 湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用. 地质力学学报, 4 (1): 63-71.

引用本文:

朱大岗, 孟宪刚, 王建平, 等, 1998. 湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用. 地质力学学报, 4 (1): 63-71.

Zhu Dagang, Meng Xiangang, Wang Jianping, et al., 1998. ON TECTONIC FEATURES OF THE MAJOR FRACTURAL ZONES AND THEIR CONTROL OF MINEROGENESIS IN THE GOLD AREA OF THE MID-XUEFENGSHAN MOUNTAIN, HUNAN PROVINCE. Journal of Geomechanics, 4 (1): 63-71.

Citation:

Zhu Dagang, Meng Xiangang, Wang Jianping, et al., 1998. ON TECTONIC FEATURES OF THE MAJOR FRACTURAL ZONES AND THEIR CONTROL OF MINEROGENESIS IN THE GOLD AREA OF THE MID-XUEFENGSHAN MOUNTAIN, HUNAN PROVINCE. Journal of Geomechanics, 4 (1): 63-71.

朱大岗, 孟宪刚, 王建平, 等, 1998. 湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用. 地质力学学报, 4 (1): 63-71.

引用本文:

朱大岗, 孟宪刚, 王建平, 等, 1998. 湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用. 地质力学学报, 4 (1): 63-71.

Zhu Dagang, Meng Xiangang, Wang Jianping, et al., 1998. ON TECTONIC FEATURES OF THE MAJOR FRACTURAL ZONES AND THEIR CONTROL OF MINEROGENESIS IN THE GOLD AREA OF THE MID-XUEFENGSHAN MOUNTAIN, HUNAN PROVINCE. Journal of Geomechanics, 4 (1): 63-71.

Citation:

Zhu Dagang, Meng Xiangang, Wang Jianping, et al., 1998. ON TECTONIC FEATURES OF THE MAJOR FRACTURAL ZONES AND THEIR CONTROL OF MINEROGENESIS IN THE GOLD AREA OF THE MID-XUEFENGSHAN MOUNTAIN, HUNAN PROVINCE. Journal of Geomechanics, 4 (1): 63-71.

湘西雪峰山中段金矿区主要断裂带构造特征及其控矿作用

1. 中国地质科学院地质力学研究所;
2. 湖南怀化地矿局;
3. 湖南地矿局四○七地质队

基金项目:

国家计委《黔阳地区金锑矿控矿条件及靶区优选》专项研究及地矿部地质力学开放研究实验室基金资助项目部分研究成果

作者简介:
朱大岗,男,1951年生,副研究员。1978年毕业于南京大学地质系矿物岩石学专业,主要从事显微构造、构造地球化学、矿田构造方面的研究工作。通讯地址:北京市海淀区民族学院南路11号地质力学研究所。邮政编码:100081。

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- 文章访问数: 283
- HTML全文浏览量: 30
- PDF下载量: 11
- 被引次数: 0
出版历程
- 收稿日期: 1997-06-23
- 修回日期: 1998-02-16
- 刊出日期: 1998-03-28

ON TECTONIC FEATURES OF THE MAJOR FRACTURAL ZONES AND THEIR CONTROL OF MINEROGENESIS IN THE GOLD AREA OF THE MID-XUEFENGSHAN MOUNTAIN, HUNAN PROVINCE

1. Institute of geomechanics, CAGS;
2. Huaihua Bureau of Geology and Mineral Resources of Hunan;
3. 407 Geological Party of Hunan Bureau of Geology and Mineral Resources

摘要: 本文论述了雪峰山中段金矿区基本构造特征及控矿作用,着重指出,NE向韧-脆性剪切带是该区主要的导矿构造,而NW向断裂带则为本区主要的容矿构造。现已探明的金矿体也均沿此方向展布。
- 雪峰山 /
- 韧-脆性断裂带 /
- 构造控矿作用
Abstract: A study of the major fracture zones in the gold-forming area of the Mid-Xuefengshan Mountain has been made by an analysis of the macrostructural features,the microstructural deformation and the tectonogeochemistry.The basic features of these zones and their control of minerogenesis are discussed in this article.The authors point out that the north east-trending ductile-brittle shear zone is the major structure as passageway for ore fluid in the gold-forming area of the Mid-Xuefengshan Mountain and that the north-west-trending fault is an important host structure along which the presently explored gold ore bodies are distributed.
- Xuefengshan /
- ductile-brittle fault /
- structural ore-controlling

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文章访问数: 283
HTML全文浏览量: 30
PDF下载量: 11
被引次数: 0

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