ATTENUATION OF BROAD-BAND (50-1500 HZ) SEISMIC-WAVES IN GRANITIC-ROCKS NEAR THE EARTHS SURFACE

We report Q-estimates from borehole-to-tunnel seismic experiments at N agra's ''Grimsel Test Site'' (GTS). The probed granitic rocks are cut by brittle faults but do not show any signs of pervasive weathering. Q -values estimated from P-wave first arrivals by the spectral ratio and rise time methods range from about 20 to 60 with a median value of 35 and a standard error of 20% or less. The surprisingly low Q-values in ferred indicate that even outside the weathering zone, seismic attenua tion in some parts of the uppermost crystalline crust may be very high .