Subducted seamount imaged in the rupture zone of the 1946 nankaido earthquake

@article{Kodaira2000SubductedSI,
  title={Subducted seamount imaged in the rupture zone of the 1946 nankaido earthquake},
  author={Kodaira and Takahashi and Nakanishi and Miura and Kaneda},
  journal={Science},
  year={2000},
  volume={289 5476},
  pages={104-6}
}
The Nankai Trough is a vigorous subduction zone where large earthquakes have been recorded since the seventh century, with a recurrence time of 100 to 200 years. The 1946 Nankaido earthquake was unusual, with a rupture zone estimated from long-period geodetic data that was more than twice as large as that derived from shorter period seismic data. In the center of this earthquake rupture zone, we used densely deployed ocean bottom seismographs to detect a subducted seamount 13 kilometers thick… CONTINUE READING
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