当サイトでは、より良いサービスを提供するため、クッキーを利用しています。クッキーの使用に同意いただける場合は「同意」ボタンをクリックし、クッキーポリシーについては「詳細を見る」をクリックしてください。詳しくは当サイトの サイトポリシー をご確認ください。

詳細を見る...
ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To

Field does not validate



インデックスリンク

インデックスツリー

  • RootNode

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "44f28423-3c0a-4c84-a4af-6e17dfd2bdd5"}, "_deposit": {"id": "2858", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "2858"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00002858", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2013-01-01", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "405", "bibliographicPageStart": "390", "bibliographicVolumeNumber": "118", "bibliographic_titles": [{"bibliographic_title": "Journal of Geophysical Research: Solid Earth", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "An Mw 9.0 great earthquake struck northeast Japan on 11 March 2011, causing crustal deformation of 1 to 2 m in volcanic areas. We applied synthetic aperture radar interferometry using Phased Array type L-band Synthetic Aperture Radar on the ALOS satellite to investigate local deformation around volcanoes associated with the earthquake. We estimated the fault-slip distribution along the trough based on obtained interferograms and crustal deformation from GEONET, and the estimated fault model explained the observed coseismic deformations well. The residual suggested local deformation around the Akita-Komagatake, Kurikoma, Zao, Azuma, and Nasu volcanoes. Their deformations were obtained from independent synthetic aperture radar pairs. Additionally, deformations in the Kurikoma, Zao, and Azuma volcanoes were confirmed by GEONET data (no GEONET stations are located in the deformation areas of other volcanoes). These facts indicate that the obtained local deformations must be actual deformations, rather than noise. Our hypothesis is that coseismic extensional deformation concentrates in the soft medium under a volcano (e.g., magma and its surrounding rock) and that this deformation has caused local deformation with subsidence. To validate this hypothesis, we carried out numerical experiments using the finite element method for a soft medium under a volcano. Distributions of observed local deformations stretch in the direction of the minor principal axis of strain, and such distributions were obtained in this experiment, indicating that the hypothesis is plausible. Conceivably, such a concentration of coseismic deformation in a magma chamber may induce a volcanic eruption. Key Points We found volcano deformations induced by the Tohoku Earthquake Volcano deformations were confirmed from independent SAR pairs and GPS It can be explained by local subsidence induced by coseismic deformation ©2012. American Geophysical Union. All Rights Reserved.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "Blackwell Publishing Ltd", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1029/2011JB009129"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "2169-9356", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "T. Ozawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "E. Fujita", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Local deformations around volcanoes associated with the 2011 off the Pacific coast of Tohoku earthquake", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Local deformations around volcanoes associated with the 2011 off the Pacific coast of Tohoku earthquake", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/2858", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-04-27"}, "publish_date": "2023-04-27", "publish_status": "0", "recid": "2858", "relation": {}, "relation_version_is_last": true, "title": ["Local deformations around volcanoes associated with the 2011 off the Pacific coast of Tohoku earthquake"], "weko_shared_id": -1}
  1. 防災科研関係論文

Local deformations around volcanoes associated with the 2011 off the Pacific coast of Tohoku earthquake

https://nied-repo.bosai.go.jp/records/2858
https://nied-repo.bosai.go.jp/records/2858
3eedbe92-079e-4255-a275-467b976d2397
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル Local deformations around volcanoes associated with the 2011 off the Pacific coast of Tohoku earthquake
言語
言語 eng
著者 T. Ozawa

× T. Ozawa

en T. Ozawa

Search repository
E. Fujita

× E. Fujita

en E. Fujita

Search repository
抄録
内容記述タイプ Other
内容記述 An Mw 9.0 great earthquake struck northeast Japan on 11 March 2011, causing crustal deformation of 1 to 2 m in volcanic areas. We applied synthetic aperture radar interferometry using Phased Array type L-band Synthetic Aperture Radar on the ALOS satellite to investigate local deformation around volcanoes associated with the earthquake. We estimated the fault-slip distribution along the trough based on obtained interferograms and crustal deformation from GEONET, and the estimated fault model explained the observed coseismic deformations well. The residual suggested local deformation around the Akita-Komagatake, Kurikoma, Zao, Azuma, and Nasu volcanoes. Their deformations were obtained from independent synthetic aperture radar pairs. Additionally, deformations in the Kurikoma, Zao, and Azuma volcanoes were confirmed by GEONET data (no GEONET stations are located in the deformation areas of other volcanoes). These facts indicate that the obtained local deformations must be actual deformations, rather than noise. Our hypothesis is that coseismic extensional deformation concentrates in the soft medium under a volcano (e.g., magma and its surrounding rock) and that this deformation has caused local deformation with subsidence. To validate this hypothesis, we carried out numerical experiments using the finite element method for a soft medium under a volcano. Distributions of observed local deformations stretch in the direction of the minor principal axis of strain, and such distributions were obtained in this experiment, indicating that the hypothesis is plausible. Conceivably, such a concentration of coseismic deformation in a magma chamber may induce a volcanic eruption. Key Points We found volcano deformations induced by the Tohoku Earthquake Volcano deformations were confirmed from independent SAR pairs and GPS It can be explained by local subsidence induced by coseismic deformation ©2012. American Geophysical Union. All Rights Reserved.
言語 en
書誌情報 en : Journal of Geophysical Research: Solid Earth

巻 118, 号 1, p. 390-405, 発行日 2013-01-01
出版者
言語 en
出版者 Blackwell Publishing Ltd
ISSN
収録物識別子タイプ ISSN
収録物識別子 2169-9356
DOI
関連識別子 10.1029/2011JB009129
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-30 09:19:47.631025
Show All versions

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3

Change consent settings


Powered by WEKO3

Change consent settings