In-situ stress measurements and regional stress field assessment in the Xinjiang candidate area for China's HLW disposal

2015 ◽  
Vol 197 ◽  
pp. 42-56 ◽  
Author(s):  
X.G. Zhao ◽  
J. Wang ◽  
X.H. Qin ◽  
M. Cai ◽  
R. Su ◽  
...  
2017 ◽  
Vol 220 ◽  
pp. 76-84 ◽  
Author(s):  
Jianju Du ◽  
Xianghui Qin ◽  
Qingli Zeng ◽  
Luqing Zhang ◽  
Qunce Chen ◽  
...  

2010 ◽  
Vol 27 (1-2) ◽  
Author(s):  
A. E. SCHEIDEGGER

The stress systems wliich are and have been active in a well-defined calcareous mountain massif (the Iloclikonig massif in Austria) have been determined: (I) f r om joint orientations in the Paleozoic basement, (II) from joint orientations in the calcareous superstructure and (III) from in situ stress measurements in a mine beneath the massif. It was found (I) t h a t t h e stresses which produced the Paleozoic joint system is quite distinct f r om t h e other systems active in the area, (II) t h a t ' t h e joints in the supers t r u c t u r e correspond to a stress system t h a t is in conformity with the general north-south thrust thought to have created the Alps and (III) that t h e stresses measured in situ represent nothing but the effect of the presentday overburden topography.


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