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This study investigates the differential crustal attenuation characteristics of the Garhwal and Kumaon Himalaya regions based on seismological and geophysical data. It finds that the Garhwal region exhibits higher shear wave velocities and lower attenuation compared to the Kumaon region, suggesting a higher seismic hazard in Garhwal. The research utilizes strong motion networks and various methodologies to analyze the frequency-dependent quality factors of seismic waves in both regions.

Author

Mohit Pandey

Language

EN