FAULT SYSTEMS IN THE QIFENGCHAN-DETIANGOU GOLD FIELD OF HUAIROU,BEIJING,AND ITS CONTROL OF GOLD MINERALIZATION

Li Zhongjian; Chen Bailin; Dong Faxian; Wang Ping'an; Wang Shifa; Li Huaiyong

Volume 4 Issue 2

Jun. 1998

Turn off MathJax

Article Contents

Article Navigation > Journal of Geomechanics > 1998 > 4(2): 21-29

Li Zhongjian, Chen Bailin, Dong Faxian, et al., 1998. FAULT SYSTEMS IN THE QIFENGCHAN-DETIANGOU GOLD FIELD OF HUAIROU,BEIJING,AND ITS CONTROL OF GOLD MINERALIZATION. Journal of Geomechanics, 4 (2): 21-29.

Citation:

PDF( 499 KB)

FAULT SYSTEMS IN THE QIFENGCHAN-DETIANGOU GOLD FIELD OF HUAIROU,BEIJING,AND ITS CONTROL OF GOLD MINERALIZATION

1. Institute of Geomechanics, CAGS;
2. Beijing Geological Survey;
3. No.1 Prospecting Party, BGMR, Beijing

More Information

Received: 1998-03-28
Revised: 1998-04-28
Published:

Abstract

Abstract

In the Qifengcha-Detiangou gold field,the N-S-trending and E-W-trending fault zones are the major ore-bearing structural zones,which are characterized by ductile-brittle deformation.Mineralization of gold is closely related to mylonites and quartz veins.Gold bodies are confined to part of fault zones where occur stronger deformation and facies changes of rock and minerals.
- gold field,
- fault system,
- control of gold mineralization