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based on densely mobile microtremor measurements, 2) evaluated sensitivity for CVs by numerical simulations for wave propagation with complex media, and 3) compared power spectral density estimated from CVs with that calculated from subsurface structure model. As a result, we found that CVs of peak periods were able to represent irregularities of sediment boundaries . 微動の水平上下スペクトル比のピーク周期の空間変動と 表層地盤の不整形性の関係 RELATIONSHIP BETWEEN IRREGULARITY OF SEDIMENT-BASEMENT INTERFACE AND SPATIAL VARIATION IN PEAK PERIODS OF HORIZONTAL-TO-VERTICAL SPECTRAL RATIO OF MICROTREMORS

nihon kenchiku gakkai kozokei ronbunshu/nihon kenchiku gakkai kōzō-kei ronbunshū

RELATIONSHIP BETWEEN IRREGULARITY OF SEDIMENT-BASEMENT INTERFACE AND SPATIAL VARIATION IN PEAK PERIODS OF HORIZONTAL-TO-VERTICAL SPECTRAL RATIO OF MICROTREMORS