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  1. 防災科研関係論文

Slip-Deficit Rate Distribution Along the Nankai Trough, Southwest Japan, With Elastic Lithosphere and Viscoelastic Asthenosphere

https://nied-repo.bosai.go.jp/records/4576
https://nied-repo.bosai.go.jp/records/4576
0961ea3b-2542-41eb-a47f-5cf1cd9f7320
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Slip-Deficit Rate Distribution Along the Nankai Trough, Southwest Japan, With Elastic Lithosphere and Viscoelastic Asthenosphere
言語
言語 eng
著者 Akemi Noda

× Akemi Noda

en Akemi Noda

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Tatsuhiko Saito

× Tatsuhiko Saito

en Tatsuhiko Saito

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Eiichi Fukuyama

× Eiichi Fukuyama

en Eiichi Fukuyama

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抄録
内容記述タイプ Other
内容記述 In southwest Japan, great earthquakes have occurred on the plate interface along the Nankai trough with a recurrence time of approximately 100years. Most previous studies estimated slip deficits on the seismogenic zone from interseismic Global Navigation Satellite System (GNSS) velocity data assuming slip-response functions for an elastic medium. The observed surface velocities, however, include effects of viscoelastic relaxation in the asthenosphere caused by slip motion associated with seismic cycles. If the elastic responses cannot adequately approximate the deformation of the viscoelastic medium, the results of an inversion analysis could be biased. If the recurrence interval is greater than the effective relaxation time in the elastic-viscoelastic layered structure, we were able to formulate an inverse problem for the estimation of slip-deficit rates from GNSS velocity data with completely relaxed slip-response functions for a later stage of the seismic cycle. Analyzing surface velocity data from GNSS daily coordinate data between March 2005 and February 2011 together with seafloor geodetic data, we estimated the slip-deficit rate distribution by the strain data inversion method. There were significant differences between the results using elastic and completely relaxed responses. Although the result with elastic responses shows a high coupling zone in the coastal region, it was located trenchward when completely relaxed responses were used. We found that the peak slip-deficit rate increases as the thickness of the lithosphere becomes thinner. Moreover, we succeeded in appropriately separating elastic-viscoelastic deformation due to plate coupling from rigid block motion.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

巻 123, 号 9, p. 8125-8142, 発行日 2018-09
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ EISSN
収録物識別子 2169-9356
DOI
関連識別子 10.1029/2018JB015515
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