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  1. 防災科研関係論文

Non-volcanic seismic swarm and fluid transportation driven by subduction of the Philippine Sea slab beneath the Kii Peninsula, Japan

https://nied-repo.bosai.go.jp/records/4988
https://nied-repo.bosai.go.jp/records/4988
44f11db0-6a4b-40de-815f-a4dff35cc512
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル Non-volcanic seismic swarm and fluid transportation driven by subduction of the Philippine Sea slab beneath the Kii Peninsula, Japan
言語
言語 eng
著者 Aitaro Kato

× Aitaro Kato

en Aitaro Kato

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Atsushi Saiga

× Atsushi Saiga

en Atsushi Saiga

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Tetsuya Takeda

× Tetsuya Takeda

en Tetsuya Takeda

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Takaya Iwasaki

× Takaya Iwasaki

en Takaya Iwasaki

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Toru Matsuzawa

× Toru Matsuzawa

en Toru Matsuzawa

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抄録
内容記述タイプ Other
内容記述 To understand the mechanism of an intensive non-volcanic seismic swarm in the Kii Peninsula, Japan, we used a dense seismic linear array to measure fine-scale variations of seismic velocities and converted teleseismic waves. A low-velocity anomaly confined to just beneath the seismic swarm area is clearly imaged, which correlates spatially with an uplifted surface area and a highly conductive and strong attenuative body. These results suggest that fluids such as partial melt or water are present beneath this non-volcanic seismic swarm area. It is notable that the island arc Moho below the seismic swarm area is at a depth of approximately 32 km in the northern part of the seismic swarm area and shallows to approximately 20 km towards the south, due to the raised structure of the serpentinized mantle wedge. In addition, we show that the hydrated oceanic crust of the subducting Philippine Sea slab is characterized by low velocities with a high Poisson's ratio at depths of less than 40 km. In contrast, dehydration conversion from oceanic basalt to eclogite takes place at depths greater than 50 km. Water released from the subducting oceanic crust could cause serpentinization of the mantle wedge and infiltration into the forearc base of the overlying plate. The interaction between dehydration of the subducting oceanic crust and hydration of the mantle wedge and overlying plate exerts an important role in driving the non-volcanic seismic swarm activity in the Kii Peninsula.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 66, 発行日 2014-08
出版者
言語 en
出版者 SPRINGER HEIDELBERG
ISSN
収録物識別子タイプ ISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/1880-5981-66-86
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