Combination of Electrical Resistivity Tomography and Seismic Refraction Methods to Characterize Sandstone Deposits

References

1. Avalos, E; Malone, D.; Peterson, Anderson, W.; Gehrels, R.
   (2016). Two-dimensional seismic refraction tomography of a buried bedrock valley at Hallsands beach, Devon, United Kingdom.Environmental Geosciences, 24(4):179–193.
   [Google Scholar]
2. Cardarelli, E.; De Donno, G.
   (2017). Multidimensional electrical resistivity survey for bedrock detection at the Rieti Plain (Central Italy.Journal of Applied Geophysics.141, 77–87.
   [Google Scholar]
3. Chambers, J.E.; Wilkinson, P.B.; Wardrop, D.; Hameed, A.; Hill, I.; Jeffrey, C.; Loke, M.H.; Meldrum, P.I.; Kuras, O.; Cave, M.; Gunn, D.A.
   (2012). Bedrock detection beneath river terrace deposits using three-dimensional electrical resistivity tomography.Geomorphology, 177–178, 17–25
   [Google Scholar]
4. Dahlin, T., Zhoo, B.
   , 2004. A numerical comparison of 2D resistivity imaging with 10 electrode arrays.Geophysical Prospecting, 52, 379–398.
   [Google Scholar]
5. De Groot-Hedlin, C., Constable, S.
   , 1990. Occam’s inversion to generate smooth, two dimensional models from magnetotelluric data.Geophysics, 55, 1613–1624.
   [Google Scholar]
6. Loke, M.H.
   , 2010. Tutorial: 2D and 3D Electrical Imaging Surveys. (154 pp).
   [Google Scholar]
7. Lucius, J.E., Lauger, W.H., and Ellefsen, K.J.
   , (2007). An introduction to using surface geophysics to characterize sand and gravel deposits, in US Geological Survey Circular, US Department of the Interior.
   [Google Scholar]