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This document reviews attenuation measurements from borehole recordings of earthquakes, highlighting the significant differences in crustal attenuation between near-surface and deeper layers. It finds that Q values are very low in the near-surface, increasing with depth, and that intrinsic attenuation dominates at seismogenic depths. The study emphasizes the importance of borehole data for understanding seismic wave propagation and the limitations of surface recordings in estimating attenuation at higher fr

Author

bizhan abgarmi

Language

EN