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

Zhu Dagang; Meng Xiangang; Wang Jianping; Tian Xiaojuan; Liu Xiangqin; Zhao Jianguang

Volume 4 Issue 1

Mar. 1998

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Article Navigation > Journal of Geomechanics > 1998 > 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.

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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

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Received: 1997-06-23
Revised: 1998-02-16
Published:

Abstract

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