Abstract In order to obtain the characteristics of in situ stress field in outburst mining area, using the hollow inclusion (HI) technique to measure the in situ stress of coal and gas outburst mining area. The measurement sites located in northeast, middle and east of china, which include eight mining areas such as Fuxin, Pingdingshan, Hebi and Huainan. Base on the analysis of measurement data from outburst mining area, conclusions could be obtained as follow: (a) major principal stress and minor principal stress is horizontal stress and interim principal stress is vertical stress, and the type of outburst area’s stress field is dynamic stress field; (b) the major principal stress and minor principal stress are higher than other regions and the tectonic stress is outstanding; and (c) the ratio of major principal and vertical stress is decrease with the increase of depth and the type of stress field is likely transfer dynamic to static. Thus, in situ stress plays a key role during the occurring and development of coal and gas outburst, which is an important reason of severe outburst in China.
[1]
E. Hoek,et al.
Trends in relationships between measured in-situ stresses and depth
,
1978
.
[2]
Liu Gao-feng.
Regional forecast of coal and gas burst based on fuzzy pattern recognition
,
2007
.
[3]
Li Shuangyang,et al.
ANALYSIS OF DISTRIBUTION RULE OF GEOSTRESS IN CHINA
,
2007
.
[4]
Stefan Bachu,et al.
In situ stress magnitude and orientation estimates for Cretaceous coal-bearing strata beneath the plains area of central and southern Alberta
,
2003
.
[5]
Li Sheng.
PATTERN RECOGNITION AND POSSIBILITY PREDICTION OF COAL AND GAS OUTBURST
,
2005
.
[6]
E. M. Anderson,et al.
The dynamics of faulting : and dyke formation with applications to Britain
,
1953,
Geological Magazine.
[7]
Lincoln Paterson,et al.
A model for outbursts in coal
,
1986
.
[8]
Guo De-yong.
Prediction method of coal and gas outburst by analytic hierarchy process and fuzzy comprehensive evaluation
,
2007
.