Estimation and correction of wavelet dispersion in ground penetrating radar data
The attenuation of electromagnetic (EM) waves in many geological materials is strongly dependent upon frequency in the ground penetrating radar (GPR) range; high frequencies are attenuated much more quickly than lower ones during propagation. For this reason, the GPR wavelet often undergoes a sig...
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| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/10414 |