A STUDY OF ORE-CONTROLLING STRUCTURES ON GOLD AND ANTIMONG IN THE MID-XUEFENG MOUNTAIN, HUNAN PROVINCE

ZHU Da-gang; MENG Xian-gang; LUO Xue-quan; WEI Dao-fang; FENG Xiang-yang; SHAO Zhao-gang; ZHAO Jian-guang; LIU Xing-qin; WANG Jian-ping; WANG Zhi-shun

2000 Vol. 6, No. 4

Article Contents

Article navigation > Journal of Geomechanics > 2000 > 6(4): 79-87

Next Article Previous Article

ZHU Da-gang, MENG Xian-gang, LUO Xue-quan, WEI Dao-fang, FENG Xiang-yang, SHAO Zhao-gang, ZHAO Jian-guang, LIU Xing-qin, WANG Jian-ping, WANG Zhi-shun. 2000. A STUDY OF ORE-CONTROLLING STRUCTURES ON GOLD AND ANTIMONG IN THE MID-XUEFENG MOUNTAIN, HUNAN PROVINCE. Journal of Geomechanics, 6(4): 79-87.

Citation:

A STUDY OF ORE-CONTROLLING STRUCTURES ON GOLD AND ANTIMONG IN THE MID-XUEFENG MOUNTAIN, HUNAN PROVINCE

1. Institute of Geomechanics, CAGS, Beijing 100081, China;
2. 407 Geological Party of Hunan Bureau of Geology and Mineral Resources, Huaihua 418000, China

Received Date: 13 July 1999

Abstract

Abstract

A study of the fabrics of ductile-brittle rock deformation during the mineralization epoch by X-ray diffraction method is made. The aim is to find out the structural control of the gold and antimony in the Mid-Xuefeng Mountain so as to predict its distribution and enrichment. The results show that the NE-trending compresso-shear structural belt may serve as the passage way for the SE-NW ore fluid flow under a stress regime with the greatest principal stress trending NW-SE, and the NW-SE trending tenso-shear structural belt associated with and derived from the NE-SW-striking structures as the host structure and described.
- ore-controlling structure /
- X-ray diffraction method /
- rock fabric /
- Xuefengshan /