scholarly journals Seismic reflection investigations of sinkholes beneath Interstate Highway 70 in Kansas

Geophysics ◽  
1986 ◽  
Vol 51 (2) ◽  
pp. 295-301 ◽  
Author(s):  
Don W. Steeples ◽  
Ralph W. Knapp ◽  
Carl D. McElwee

Seismic reflection studies were performed across actively developing sinkholes located astride Interstate Highway 70 in Russell County, Kansas. Results indicate that high‐resolution seismic reflection surveys are useful in the subsurface investigation of some sinkholes. In particular, we were able to delineate the subsurface vertical and horizontal extent of the sinkholes because of the excellent acoustical marker‐bed characteristics of the Stone Corral anhydrite. The seismic reflection evidence presented here, combined with borehole information from 1967, suggest that the Stone Corral anhydrite has been down‐dropped within one of the sinkholes as much as 30 m in 13 years. The seismic reflection method is potentially useful in engineering studies of other sinkholes and karst features. The seismic data presented here were obtained in the presence of relatively heavy highway traffic (i.e., up to a few dozen vehicles per minute) using the MiniSOSIE recording technique.

2013 ◽  
Vol 2013 (1) ◽  
pp. 1-6
Author(s):  
Ayman N. Qadrouh ◽  
Abdulrahman G. Alanezi ◽  
Ibraheem K. Hafiz ◽  
Khyzer Munir ◽  
Mazen M. ALyousif

Geophysics ◽  
1992 ◽  
Vol 57 (10) ◽  
pp. 1373-1380 ◽  
Author(s):  
Richard D. Miller ◽  
Victor Saenz ◽  
Robert J. Huggins

The common‐depth‐point (CDP) seismic‐reflection method was used to delineate subsurface structure in a 3-m thick, 220-m deep coal zone in the Palau area of Coahuila, Mexico. An extensive series of walkaway‐noise tests was performed to optimize recording parameters and equipment. Reflection events can be interpreted from depths of approximately 100 to 300 m on CDP stacked seismic sections. The seismic data allow accurate identification of the horizontal location of the structure responsible for a drill‐discovered 3-m difference in coal‐zone depth between boreholes 150 m apart. The reflection method can discriminate folding with wavelengths in excess of 20 m and faulting with offset greater than 2 m at this site.


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