High-density surveys conducted to reveal active deformations of the upper forearc slope along the Ryukyu Trench, western Pacific, Japan

Author:

Arai KohsakuORCID,Inoue Takahiko,Sato Tomoyuki

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference43 articles.

1. Amante C, Eakins BW (2009) ETOPO1 1 arc-minute global relief model: procedures, data sources and analysis. NOAA Technical Memorandum NESDIS NGDC-24, National Oceanic and Atmospheric Administration (NOAA), Washington, DC.

2. Ando M, Nakamura M, Matsumoto T, Furukawa M, Tadokoro K, Furumuto M (2009) Is the Ryukyu subduction zone in Japan coupled or decoupled? —the necessity of seafloor crustal deformation observation. Earth Planets Space 61:1031–1039.

3. Arai K, Inoue T, Ikehara K, Sasaki T (2014) Episodic subsidence and active deformation of the forearc slope along the Japan Trench near the epicenter of the 2011 Tohoku Earthquake. Earth Planet Sci Lett 408:9–15. https://doi.org/10.1016/j.epsl.2014.09.048 .

4. Arai K, Inoue T, Sato T (in press) Geological map of the vicinity of southern Okinawa-Jima island. Marine Geology Map Series 90 (CD). Geological Survey of Japan, AIST. (in Japanese with English abstract).

5. Arai K, Inoue T, Sato T, TuZino T, Murakami F (2010) 16ch high-resolution seismic reflection surveys on the active fault of upper fore-arc slope off Okinawa Island, central Ryukyu Island Arc, Southwest Japan, in: AGU Fall Meeting T22A-06.

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