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  1. 防災科研関係論文

Rapid ground deformation of the Miyakejima volcano on 26-27 June 2000 detected by kinematic GPS analysis

https://nied-repo.bosai.go.jp/records/3067
https://nied-repo.bosai.go.jp/records/3067
cc042d87-443f-4103-9935-0246168cf17c
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Rapid ground deformation of the Miyakejima volcano on 26-27 June 2000 detected by kinematic GPS analysis
タイトル
言語 en
タイトル Rapid ground deformation of the Miyakejima volcano on 26-27 June 2000 detected by kinematic GPS analysis
言語
言語 eng
著者 Irwan Meilano

× Irwan Meilano

ja Irwan Meilano

en Irwan Meilano

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Kimata Fumiaki

× Kimata Fumiaki

ja Kimata Fumiaki

en Kimata Fumiaki

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Fujii Naoyuki

× Fujii Naoyuki

ja Fujii Naoyuki

en Fujii Naoyuki

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Nakao Shigeo

× Nakao Shigeo

ja Nakao Shigeo

en Nakao Shigeo

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Watanabe Hidehumi

× Watanabe Hidehumi

ja Watanabe Hidehumi

en Watanabe Hidehumi

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Sakai Shinichi

× Sakai Shinichi

ja Sakai Shinichi

en Sakai Shinichi

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Ukawa Motoo

× Ukawa Motoo

ja Ukawa Motoo

en Ukawa Motoo

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Fujita Eisuke

× Fujita Eisuke

ja Fujita Eisuke

en Fujita Eisuke

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Kawai Koji

× Kawai Koji

ja Kawai Koji

en Kawai Koji

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抄録
内容記述タイプ Other
内容記述 A kinematic GPS analysis of data from the Miyakejima volcano captured a fast developing deformation event on 26-27 June 2000 in unprecedented spatial and temporal detail. Initial ground deformation toward east and upward was observed in the southeastern part of the volcano at 18 : 00 on 26 June 2000, almost simultaneous with earthquake swarms. Some time after 21 : 30 on 26 June 2000 the displacements at these sites turned from eastward to westward. Three hours later the displacement rates increased gradually at GPS sites in the western part of Miyakejima as the seismicity migrated and approached the west coast, and reached a climax with submarine eruption at 09 : 00 on 27 June 2000. A Genetic Algorithm was used to explore the parameter space and to find the best fitting source geometry. This analysis leads to an interpretation that the 18 : 00 26 June earthquake swarm was caused by a dike intrusion near the Oyama crater. Starting from 21 : 30 this dike deflated and a new dike intruded near the west coast. Following the propagation of this dike to the offshore, a spherical source began deflating in the southwest of Oyama crater.
言語 ja
抄録
内容記述タイプ Other
内容記述 A kinematic GPS analysis of data from the Miyakejima volcano captured a fast developing deformation event on 26-27 June 2000 in unprecedented spatial and temporal detail. Initial ground deformation toward east and upward was observed in the southeastern part of the volcano at 18 : 00 on 26 June 2000, almost simultaneous with earthquake swarms. Some time after 21 : 30 on 26 June 2000 the displacements at these sites turned from eastward to westward. Three hours later the displacement rates increased gradually at GPS sites in the western part of Miyakejima as the seismicity migrated and approached the west coast, and reached a climax with submarine eruption at 09 : 00 on 27 June 2000. A Genetic Algorithm was used to explore the parameter space and to find the best fitting source geometry. This analysis leads to an interpretation that the 18 : 00 26 June earthquake swarm was caused by a dike intrusion near the Oyama crater. Starting from 21 : 30 this dike deflated and a new dike intruded near the west coast. Following the propagation of this dike to the offshore, a spherical source began deflating in the southwest of Oyama crater.
言語 en
書誌情報 ja : Earth, Planets and Space
en : Journal of geomagnetism and geoelectricity

巻 55, 号 6, p. e13-e16, 発行日 2003
出版者
言語 ja
出版者 The Seismological Society of Japan, Society of Geomagnetism and Earth, Planetary and Space Sciences, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences
出版者
言語 en
出版者 The Seismological Society of Japan, Society of Geomagnetism and Earth, Planetary and Space Sciences, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences
ISSN
収録物識別子タイプ ISSN
収録物識別子 1343-8832
DOI
関連識別子 10.1186/BF03351761
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