G. Grandjean et Jc. Gourry, GPR DATA-PROCESSING FOR 3D FRACTURE MAPPING IN A MARBLE QUARRY (THASSOS, GREECE), Journal of applied geophysics, 36(1), 1996, pp. 19-30
Ground Penetrating Radar (GPR) has been successfully applied to detect
and map fractures in marble quarries. The aim was to distinguish quic
kly intact marketable marble areas from fractured ones in order to imp
rove quarry management. The GPR profiling method was chosen because it
is non destructive and quickly provides a detailed image of the subsu
rface. It was performed in domains corresponding to future working are
as in real quarry-exploitation conditions. Field surveying and data pr
ocessing were adapted to the local characteristics of the fractures: E
-W orientation, sub-vertical dip, and karst features. After the GPR pr
ofiles had been processed, using methods adapted from seismics (amplit
ude compensation, filtering and Fourier migration), the interpreted fr
actures from a 12 x 24 x 15 m zone were incorporated into a 3D model.
Due to the low electrical conductivity of the marble, GPR provides pen
etration depths of about 8 and 15 m, and resolutions of about 1 and 5
cm for frequencies of 900 and 300 MHz respectively. The detection powe
r thus seems to be sufficient to recommend use of this method. As requ
ested by the quarriers, the 3D representation can be used directly by
themselves to locate high- or low-quality marble areas. Comparison bet
ween the observed surface fractures and the fractures detected using G
PR showed reasonable correlation.