Seismic Wavefields in the Deep Seafloor Area from a Submarine Landslide Source

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• 作者：Takeshi Nakamura (1)
  Hiroshi Takenaka (2) (4)
  Taro Okamoto (3)
  Yoshiyuki Kaneda (1)
  
• 关键词：DONET ; landslide ; seismic wave propagation ; finite difference method ; seafloor observation ; tonankai area
• 刊名：Pure and Applied Geophysics
• 出版年：2014
• 出版时间：July 2014
• 年：2014
• 卷：171
• 期：7
• 页码：1153-1167
• 全文大小：3,832 KB
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• 作者单位：Takeshi Nakamura (1)
  Hiroshi Takenaka (2) (4)
  Taro Okamoto (3)
  Yoshiyuki Kaneda (1)
  
  1. Earthquake and Tsunami Research Project for Disaster Prevention, Japan Agency for Marine-Earth Science and Technology, 3173-25 Showa-machi, Kanazawa-ku, Yokohama 236-0001, Japan
  2. Department of Earth and Planetary Sciences, Kyushu University, 6-10-1 Hakozaki, Higashi-ku, 812-8581, Japan
  4. Department of Earth Sciences, Okayama University, 3-1-1 Tsushima-Naka, Kita-ku, Okayama 700-8530, Japan
  3. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8551, Japan
  
• ISSN：1420-9136

文摘

We use the finite difference method to simulate seismic wavefields at broadband land and seafloor stations for a given terrestrial landslide source, where the seafloor stations are located at water depths of 1,900-,300?m. Our simulation results for the landslide source explain observations well at the seafloor stations for a frequency range of 0.05-.1?Hz. Assuming the epicenter to be located in the vicinity of a large submarine slump, we also model wavefields at the stations for a submarine landslide source. We detect propagation of the Airy phase with an apparent velocity of 0.7?km/s in association with the seawater layer and an accretionary prism for the vertical component of waveforms at the seafloor stations. This later phase is not detected when the structural model does not consider seawater. For the model incorporating the seawater, the amplitude of the vertical component at seafloor stations can be up to four times that for the model that excludes seawater; we attribute this to the effects of the seawater layer on the wavefields. We also find that the amplification of the waveform depends not only on the presence of the seawater layer but also on the thickness of the accretionary prism, indicating low amplitudes at the land stations and at seafloor stations located near the trough but high amplitudes at other stations, particularly those located above the thick prism off the trough. Ignoring these characteristic structures in the oceanic area and simply calculating the wavefields using the same structural model used for land areas would result in erroneous estimates of the size of the submarine landslide and the mechanisms underlying its generation. Our results highlight the importance of adopting a structural model that incorporates the 3D accretionary prism and seawater layer into the simulation in order to precisely evaluate seismic wavefields in seafloor areas.