Studying the effects of gypsum karst cavities in tunneling

Author(s):  
M.R. Al Kaabi ◽  
R.L. Sousa
Keyword(s):  
2002 ◽  
Vol 17 (2) ◽  
pp. 134-141 ◽  
Author(s):  
J. M. Calaforra ◽  
A. Pulido-Bosch ◽  
M. Lopez-Chicano

2018 ◽  
Vol 35 ◽  
pp. 03002 ◽  
Author(s):  
Sławomir Porzucek ◽  
Monika Łój ◽  
Karolina Matwij ◽  
Wojciech Matwij

In the region of Siesławice (near Busko-Zdrój, Poland) there are unique phenomena of gypsum karst. Atmospheric factors caused numerous gypsum outcrops, canals and underground voids. The article presents the possibility of using non-invasive gravimetric surveys supplemented with geodetic measurements to illustrate karst changes occurring around the void. The use of modern geodetic measurement techniques including terrestrial and airborne laser scanning enables to generate a digital terrain model and a three-dimensional model of voids. Gravimetric field studies allowed to map the anomalies of the gravitational field of the near-surface zone. Geodetic measurement results have made it possible to accurately determine the terrain correction that supplemented the gravimetric anomaly information. Geophysical interpretation indicate the presence of weathered rocks in the near surface zone and fractures and loosened zones located surround the karst cave.


1996 ◽  
Vol 25 (3/4) ◽  
pp. 145-156 ◽  
Author(s):  
Alexander Klimchouk ◽  
Vjacheslav Andrejchuk

1996 ◽  
Vol 25 (3/4) ◽  
pp. 239-250 ◽  
Author(s):  
Paolo Forti ◽  
Ugo Sauro
Keyword(s):  

1984 ◽  
Vol 21 (8) ◽  
pp. 949-959 ◽  
Author(s):  
Po C. Tsui ◽  
David M. Cruden

An escarpment formed by the carbonate Keg River and evaporitic Chinchaga formations of Middle Devonian age extends southwards from the Slave River 30 km west of Fort Smith, Northwest Territories. Newly described folds in the bedrock are due to hydration of the anhydrite to gypsum in the Chinchaga Formation underlying the escarpment. Local groundwater flow has also dissolved subsurface cavities in the Chinchaga Formation. As these openings grew, the carbonates of the Keg River Formation subsided along stepped normal faults. Depressions within the fault blocks occurred where subsidence was concentrated along joints.


2009 ◽  
Vol 59 (5) ◽  
pp. 1057-1063 ◽  
Author(s):  
Tomás Rodríguez-Estrella ◽  
Antonio Pulido-Bosch
Keyword(s):  

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