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        <datestamp>2026-09-30T03:47:04Z</datestamp>
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          <dc:title>Additional file 2 of Quantifying the 1D explainability of low-variability and poor-misfit site responses via S-wave velocity inversion for site amplification factors</dc:title>
          <dc:creator>Ziqian Wang (25140867)</dc:creator>
          <dc:creator>Hiroshi Kawase (2358493)</dc:creator>
          <dc:creator>Yuanming Lai (8366955)</dc:creator>
          <dc:creator>Kenichi Nakano (11971855)</dc:creator>
          <dc:creator>Jikai Sun (12474355)</dc:creator>
          <dc:subject>Space Science</dc:subject>
          <dc:subject>Medicine</dc:subject>
          <dc:subject>Cell Biology</dc:subject>
          <dc:subject>Genetics</dc:subject>
          <dc:subject>Mathematical Sciences not elsewhere classified</dc:subject>
          <dc:subject>Hematology</dc:subject>
          <dc:subject>Site response</dc:subject>
          <dc:subject>1D explainability</dc:subject>
          <dc:subject>S-wave velocity inversion</dc:subject>
          <dc:subject>Horizontal site amplification factor</dc:subject>
          <dc:subject>KiK-net</dc:subject>
          <dc:subject>Particle swarm optimization</dc:subject>
          <dc:subject>Surface-to-borehole spectral ratio</dc:subject>
          <dc:description>Additional file 2. Representative waveform and corresponding FAS. Representative horizontal earthquake waveforms and corresponding FAS illustrating the waveform processing procedure used in the GIT. The figure shows the NS and EW components of waveform, S-wave onset, S-wave processing window with a 2-s cosine taper applied at both ends, and the corresponding FAS of NS and EW components. The horizontal FAS was calculated as the root-mean-square of the NS and EW components and smoothed using a Parzen window with a bandwidth of 0.1 Hz.</dc:description>
          <dc:date>2026-09-29T05:00:00Z</dc:date>
          <dc:type>Text</dc:type>
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          <dc:identifier>10.6084/m9.figshare.34029120.v1</dc:identifier>
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