| Co-Investigator(Kenkyū-buntansha) |
寺川 寿子 名古屋大学, 環境学研究科, 講師 (30451826)
伊藤 武男 名古屋大学, 環境学研究科, 准教授 (40377982)
佐々木 圭一 金沢学院大学, 基礎教育機構, 准教授 (50340021)
鷺谷 威 名古屋大学, 減災連携研究センター, 教授 (50362299)
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| Budget Amount *help |
¥18,200,000 (Direct Cost: ¥14,000,000、Indirect Cost: ¥4,200,000)
Fiscal Year 2017: ¥3,380,000 (Direct Cost: ¥2,600,000、Indirect Cost: ¥780,000)
Fiscal Year 2016: ¥2,990,000 (Direct Cost: ¥2,300,000、Indirect Cost: ¥690,000)
Fiscal Year 2015: ¥3,510,000 (Direct Cost: ¥2,700,000、Indirect Cost: ¥810,000)
Fiscal Year 2014: ¥2,860,000 (Direct Cost: ¥2,200,000、Indirect Cost: ¥660,000)
Fiscal Year 2013: ¥5,460,000 (Direct Cost: ¥4,200,000、Indirect Cost: ¥1,260,000)
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| Outline of Final Research Achievements |
In the subduction zone with back-arc expansion, crustal deformation was observed both effects due to the subducted oceanic plate and expansion of back-arc. In order to identify each component of crustal deformations, we carry out GNSS observation at Yoktoshima and leveling survey in Kikaijima island. As result, we obtain the spatial distribution of interplate coupling and tilt vector at the kikai island. In addition, we estimate 6000 BP at highest marine terrace in north region of Kikaijima island by the geological survey. As a result of modeling for the survey result and the occurrence interval of the past earthquakes using two dimensional finite element method, we obtain that the long-term uplift at kikai-jima is explained by by the geometry of subduction plate. In order to understand the time evolution of vertical deformation, we reveal that the viscoelastic structure at the mantle wedge have important role.
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