Identifying causes of ground-penetrating radar reflections using time-domain reflectometry and sedimentological analyses
Ground‐penetrating radar (GPR) is a geophysical technique widely used to study the shallow subsurface and identify various sediment features that reflect electromagnetic waves. However, little is known about the exact cause of GPR reflections because few studies have coupled wave theory to petrophys...
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Veröffentlicht in: | Sedimentology 2000-04, Vol.47 (2), p.435-449 |
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Sprache: | eng |
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