Fig. 8From: Estimation of 1-D velocity models beneath strong-motion observation sites in the Kathmandu Valley using strong-motion records from moderate-sized earthquakes1-D velocity models for four fixed sites. The model for KTP was considered as a bedrock site overlain by a layer of weathered rock and those for TVU, PTN, and THM are adjusted 1-D velocity models. Site THM has the thickest sediment. The black dashed lines indicate the initial velocity model prepared based on geological maps, cross-sections, and available borehole dataBack to article page