Characterization of Abandoned Mine Voids Under Roadway with Land-Streamer Seismic Waves

Author(s):  
Brian Sullivan ◽  
Khiem T. Tran ◽  
Brian Logston
Geophysics ◽  
2007 ◽  
Vol 72 (5) ◽  
pp. M7-M15 ◽  
Author(s):  
Daniel J. Yancey ◽  
Matthias G. Imhof ◽  
John E. Feddock ◽  
Tod Gresham

Two in-seam reflection surveys and one transmission survey were acquired at an abandoned underground mine near Hurley, Virginia, to demonstrate the feasibility of detecting abandoned-mine voids utilizing coal-seam seismic waves. Standard, commonly available tools for seismic reflection processing were used. The mine was detected and located by using trapped coal-seam seismic waves observed in both the transmission and reflection data. Detecting the void, however, was not good enough to replace drilling entirely. We conclude that in-seam seismic methods can be used for detection; but if a potential void is detected, focused drilling should be applied for accurate mapping and to circumvent potentially hazardous areas.


2012 ◽  
Vol 61 (3) ◽  
pp. 611-623 ◽  
Author(s):  
Diego Arosio ◽  
Laura Longoni ◽  
Monica Papini ◽  
Luigi Zanzi

2018 ◽  
Vol 232 ◽  
pp. 135-146 ◽  
Author(s):  
Tomás Martín-Crespo ◽  
David Gómez-Ortiz ◽  
Silvia Martín-Velázquez ◽  
Pedro Martínez-Pagán ◽  
Cristina De Ignacio ◽  
...  

Science ◽  
2014 ◽  
Vol 345 (6192) ◽  
pp. 80-82 ◽  
Author(s):  
F. Brenguier ◽  
M. Campillo ◽  
T. Takeda ◽  
Y. Aoki ◽  
N. M. Shapiro ◽  
...  

Volcanic eruptions are caused by the release of pressure that has accumulated due to hot volcanic fluids at depth. Here, we show that the extent of the regions affected by pressurized fluids can be imaged through the measurement of their response to transient stress perturbations. We used records of seismic noise from the Japanese Hi-net seismic network to measure the crustal seismic velocity changes below volcanic regions caused by the 2011 moment magnitude (Mw) 9.0 Tohoku-Oki earthquake. We interpret coseismic crustal seismic velocity reductions as related to the mechanical weakening of the pressurized crust by the dynamic stress associated with the seismic waves. We suggest, therefore, that mapping seismic velocity susceptibility to dynamic stress perturbations can be used for the imaging and characterization of volcanic systems.


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