Abstract: Three-Dimensional Hydrogeologic Characterization of Fractured Carbonate Aquifers Using Ground-Penetrating Radar

AAPG Bulletin ◽  
1998 ◽  
Vol 82 (1998) ◽  
Author(s):  
TSOFLIAS, GEORGIOS P., and JOHN M.
Keyword(s):  
Ground Penetrating Radar ◽  
Three Dimensional ◽  
Carbonate Aquifers ◽  
Fractured Carbonate ◽  
Ground Penetrating

Three‐ Dimensional Characterization of Archaeological Sites Using Multi‐Channel Ground Penetrating Radar Arrays; Benefits and Examples

2011 ◽  
Author(s):  
Kevin Hon ◽  
Scott Harris ◽  
Maureen Hays ◽  
Kimberly Pyszka
Keyword(s):  
Ground Penetrating Radar ◽  
Three Dimensional ◽  
Archaeological Sites ◽  
Ground Penetrating

scholarly journals Characterization of tillage effects on the spatial variation of soil properties using ground-penetrating radar and electromagnetic induction

Geoderma ◽  
2013 ◽  
Vol 207-208 ◽  
pp. 310-322 ◽  
Author(s):  
François Jonard ◽  
Mohammad Mahmoudzadeh ◽  
Christian Roisin ◽  
Lutz Weihermüller ◽  
Frédéric André ◽  
...  
Keyword(s):  
Soil Properties ◽  
Spatial Variation ◽  
Ground Penetrating Radar ◽  
Electromagnetic Induction ◽  
Ground Penetrating

scholarly journals Delineating shallow Neogene deformation structures in northeastern Pará State using Ground Penetrating Radar

2003 ◽  
Vol 75 (2) ◽  
pp. 235-248 ◽  
Author(s):  
Dilce F. Rossetti
Keyword(s):  
Ground Penetrating Radar ◽  
Structural Models ◽  
Field Studies ◽  
Strike Slip ◽  
Brittle Deformation ◽  
Shallow Subsurface ◽  
Deformation Structures ◽  
Ground Penetrating ◽  
Slip Motion

The geological characterization of shallow subsurface Neogene deposits in northeastern Pará State using Ground Penetrating Radar (GPR) revealed normal and reverse faults, as well as folds, not yet well documented by field studies. The faults are identified mostly by steeply-dipping reflections that sharply cut the nearby reflections causing bed offsets, drags and rollovers. The folds are recognized by reflections that are highly undulating, configuring broad concave and convex-up features that are up to 50 m wide and 80 to 90 ns deep. These deformation structures are mostly developed within deposits of Miocene age, though some of the faults might continue into younger deposits as well. Although the studied GPR sections show several diffractions caused by trees, differential degrees of moisture, and underground artifacts, the structures recorded here can not be explained by any of these ''noises''. The detailed analysis of the GPR sections reveals that they are attributed to bed distortion caused by brittle deformation and folding. The record of faults and folds are not widespread in the Neogene deposits of the Bragantina area. These GPR data are in agreement with structural models, which have proposed a complex evolution including strike-slip motion for this area from the Miocene to present.

Characterization Of A Beach Revetment Using Ground Penetrating Radar And MASW

2008 ◽  
Author(s):  
Mario Carnevale ◽  
Jutta Hager
Keyword(s):  
Ground Penetrating Radar ◽  
Ground Penetrating

Ground-Penetrating Radar Detection and Three-Dimensional Mapping of Lateral Macropores: I. Calibration

2011 ◽  
Vol 75 (4) ◽  
pp. 1226-1235 ◽  
Author(s):  
Kevin H. Gormally ◽  
Marla S. McIntosh ◽  
Anthony N. Mucciardi
Keyword(s):  
Ground Penetrating Radar ◽  
Three Dimensional ◽  
Radar Detection ◽  
Three Dimensional Mapping ◽  
Ground Penetrating ◽  
Dimensional Mapping

The non-invasive characterization of pumping-induced dewatering using ground penetrating radar

2003 ◽  
Vol 281 (1-2) ◽  
pp. 55-69 ◽  
Author(s):  
Michael J. Bevan ◽  
Anthony L. Endres ◽  
David L. Rudolph ◽  
Gary Parkin
Keyword(s):  
Ground Penetrating Radar ◽  
Non Invasive ◽  
Ground Penetrating

Three‐Dimensional Ground‐Penetrating Radar Imaging Through Multilayered Subsurface

Radio Science ◽  
2019 ◽  
Vol 54 (8) ◽  
pp. 728-737 ◽  
Author(s):  
Wenji Zhang ◽  
Ahmad Hoorfar ◽  
Qiang An
Keyword(s):  
Ground Penetrating Radar ◽  
Three Dimensional ◽  
Radar Imaging ◽  
Ground Penetrating
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