THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG

LIU Du Juan; GUO Tao; LU Gu-xian

Volume 7 Issue 3

Sep. 2001

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Article Navigation > Journal of Geomechanics > 2001 > 7(3): 245-253

FU Xue-hai, QIN Yong, LI Gui-zhong, et al., 2001. AN ANALYSIS ON THE PRINCIPAL CONTROL FACTOR OF COAL RESERVOIR PERMEABILITY iN CENTRAL AND SOUTHERN QINSHUI BASIN,SHANXI. Journal of Geomechanics, 7 (1): 45-52.

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LIU Du Juan, GUO Tao, LU Gu-xian, 2001. THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG. Journal of Geomechanics, 7 (3): 245-253.

Citation:

LIU Du Juan, GUO Tao, LU Gu-xian, 2001. THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG. Journal of Geomechanics, 7 (3): 245-253.

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THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG

Institute of Geomechanics, CAGS, Beijing 100081, China

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Abstract

Abstract

The space distributions of differential stress and principal stress in Fushan gold field are got from measuring tectonic differential stress value.Results show that the gold orebodies are always located in the areas where the tectonic stress value varies highly,not the minimum or maximum.Based on strain measurement and analysis of susceptibility anisotropy,the tectonic strain fields of the diagenetic and mineralization periods in Fushan gold field are given respectively.There was a transition of stress field from NW trending compression to NE trending compression during mineralization,and the tectonic environment of minerallization was changed from shear compress to shear -extension.
- Fushan gold field,
- tectonic stress field,
- tectonic strain field,
- transition of stress field,
- interfacial metallogenesis

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THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG

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