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- W2315205328 abstract "Authors of this document have performed several geophysical investigations within the eastern United States. Most of this experience has involved subsurface investigations in carbonate rock units. As compared with different geophysical techniques including micro gravity, electromagnetics, ground penetrating radar, spontaneous potential, and other methods, the best results in characterizing subsurface conditions in karst terrain were accomplished using surface resistivity imaging. The following discussion is based on two case studies, both involving two-dimensional and theedimensional surface resistivity surveys performed over Paleozoic age carbonate rocks in northern Virginia and West Virginia. The purpose of this document is to show the benefits and pitfalls of twodimensional and three-dimensional resistivity imaging used to characterize subsurface conditions in the karst terrain. Both methods are compared based on different site geologies, array geometries, and target size and depth. A short discussion of dipole-dipole method commonly used in two-dimensional arrays, versus pole-pole used in three-dimensional arrays is presented to indicate differences in expected data resolution. The intention of this document was also to highlight the importance of volumetric visualization of three-dimensional data sets for analysis and interpretations. Creating volumetric three-dimensional models of resistivity is useful in evaluating the location, orientation and character of potential fracture systems within relatively uniform rock masses." @default.
- W2315205328 created "2016-06-24" @default.
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- W2315205328 date "2001-01-01" @default.
- W2315205328 modified "2023-09-27" @default.
- W2315205328 title "Mapping Karst Conditions Using 2D And 3D Resistivity Imaging Methods" @default.
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- W2315205328 doi "https://doi.org/10.3997/2214-4609-pdb.192.gtv_1" @default.
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