S-wave anisotropy revealed by airgun seismic surveys using cabled seafloor seismometers in the Nankai Trough, Japan

Author(s): Kimura, T.; Araki, E.; Mikada, H.; Kodaira, S.; Miura, S.; Takahashi, N.; Takaesu, M.; Nakano, M.; Machida, Y.
Author Affiliation(s): Primary:
Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan
Other:
Kyoto University, Kyoto, Japan
Volume Title: AGU 2015 fall meeting
Source: American Geophysical Union Fall Meeting, Vol.2015; American Geophysical Union 2015 fall meeting, San Francisco, CA, Dec. 14-18, 2015. Publisher: American Geophysical Union, Washington, DC, United States
Note: In English
Summary: In the Nankai Trough, Japan, a cabled real-time seismic, geodetic and tsunami observation system, comprising twenty DONET1 seafloor and one IODP C0002G borehole observatories, monitors seismic activity above the seismogenic zone, where mega-thrust earthquakes occur at 100-150 years interval. On Nov. 2013 through June 2015, we conducted three seismic airgun surveys above DONET1 and C0002G seismometers. In this study, we aimed to reveal spatial distribution of S-wave anisotropy, i.e., a proxy of stress state governing the fault dynamics in the subduction zone, from the dataset recorded by the cabled system during these surveys In these surveys, airgun shootings at circular survey lines around each observatory with different radii of 3, 7 and 10 km were carried out. In the observed horizontal components for each shot from 3 km radius lines (R3 lines), seismic waveforms in 3.0 to 5.0s after the shot are clearly visible to indicate the up-coming P-S converted waves from the bottom of the shallow sediment, although signal-to-noise ratio decreases with depth due to spherical divergence and to complicated structure such as dipping reflectors. We computed radial and transverse records for each shot-receiver azimuth, and then estimated S-wave anisotropy parameters, i.e., magnitude and azimuth, as a function of depth for R3 lines at thirteen observatories. The obtained results confirm that the distributions of S-wave anisotropy, especially in shallow sediments, have localities: the magnitude of S-wave anisotropy becomes smaller in landward basin than in imbricated thrust zone. The axes of fast S-wave symmetry become closer to subduction direction for results from deep reflections. We plan to conduct more attentive analysis, including error evaluation using repeated shooting dataset to discuss the detectability of temporal change of S-wave anisotropy deepen the present discussion after integrating numerical analysis in complicated structure model with the current method.
Year of Publication: 2015
Research Program: IODP Integrated Ocean Drilling Program
Key Words: 18 Geophysics, Solid-Earth; Anisotropy; Body waves; Elastic waves; Geophysical methods; Geophysical surveys; IODP Site C0002; Integrated Ocean Drilling Program; Kumano Basin; NanTroSEIZE; Nankai Trough; North Pacific; Northwest Pacific; Pacific Ocean; S-waves; Seismic methods; Seismic waves; Surveys; West Pacific
Coordinates: N331800 N331801 E1363801 E1363800
Record ID: 2016045071
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