Weak interplate coupling beneath the subduction zone off Fukushima, NE Japan, inferred from GPS/acoustic seafloor geodetic observation

We have been carrying out GPS/acoustic seafloor geodetic observations at several reference points situated along the Japan Trench, a major plate boundary of subduction. A time series of horizontal coordinates of one of the seafloor reference points, located off Fukushima, obtained from seven campaig...

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Veröffentlicht in:Earth, planets, and space planets, and space, 2008-01, Vol.60 (6), p.e9-e12
Hauptverfasser: Matsumoto, Yoshihiro, Ishikawa, Tadashi, Fujita, Masayuki, Sato, Mariko, Saito, Hiroaki, Mochizuki, Masashi, Yabuki, Tetsuichiro, Asada, Akira
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container_end_page e12
container_issue 6
container_start_page e9
container_title Earth, planets, and space
container_volume 60
creator Matsumoto, Yoshihiro
Ishikawa, Tadashi
Fujita, Masayuki
Sato, Mariko
Saito, Hiroaki
Mochizuki, Masashi
Yabuki, Tetsuichiro
Asada, Akira
description We have been carrying out GPS/acoustic seafloor geodetic observations at several reference points situated along the Japan Trench, a major plate boundary of subduction. A time series of horizontal coordinates of one of the seafloor reference points, located off Fukushima, obtained from seven campaign observations for the period 2002-2008, exhibits a linear trend with a scattering root mean square of about 3 cm. A linear fit to the time series gives an intraplate crustal movement velocity of 3.1 cm per year in a westerly direction, which is significantly smaller than that at the other seafloor reference point 120 km away along the trench axis. This result implies weak interplate coupling in this region.
doi_str_mv 10.1186/BF03353114
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subjects Cosmochemistry. Extraterrestrial geology
E-Letter
Earth and Environmental Science
Earth Sciences
Earth, ocean, space
Exact sciences and technology
Geology
Geophysics/Geodesy
title Weak interplate coupling beneath the subduction zone off Fukushima, NE Japan, inferred from GPS/acoustic seafloor geodetic observation
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