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": "6fe00dc6-7cb0-48d7-a006-3131ee0995a8"}, "_deposit": {"id": "4458", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4458"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004458", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2002-05"}, "bibliographicIssueNumber": "9", "bibliographicPageStart": "1329", "bibliographicVolumeNumber": "29", "bibliographic_titles": [{"bibliographic_title": "GEOPHYSICAL RESEARCH LETTERS", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "[1] From a temporal deployment of a broadband seismic network at Usu volcano, Japan, we observed long-period (12 sec) volcanic tremors during the first few weeks of the eruptive activity which started in the end of March, 2000. The source of these long period tremors are located relatively deep at a depth of 5 km, and their amplitude variation well correlates with the uplift rate of the eruption area. We thus attribute these long period tremors to the flow induced vibration of a magma chamber and its outlet located around the source region of the long period tremors. This may be the first seismological detection of long-period (\u0026gt; 10 sec) vibrations of a deep magma plumbing system.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "AMER GEOPHYSICAL UNION", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1029/2001GL013996"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1944-8007", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "M Yamamoto", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "H Kawakatsu", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "K Yomogida", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "J Koyama", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Long-period (12 sec) volcanic tremor observed at Usu 2000 eruption: Seismological detection of a deep magma plumbing system", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Long-period (12 sec) volcanic tremor observed at Usu 2000 eruption: Seismological detection of a deep magma plumbing system", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4458", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4458", "relation": {}, "relation_version_is_last": true, "title": ["Long-period (12 sec) volcanic tremor observed at Usu 2000 eruption: Seismological detection of a deep magma plumbing system"], "weko_shared_id": -1}
  1. 防災科研関係論文

Long-period (12 sec) volcanic tremor observed at Usu 2000 eruption: Seismological detection of a deep magma plumbing system

https://nied-repo.bosai.go.jp/records/4458
https://nied-repo.bosai.go.jp/records/4458
badb7460-aa15-4813-8cc6-cad19d3fbc0b
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Long-period (12 sec) volcanic tremor observed at Usu 2000 eruption: Seismological detection of a deep magma plumbing system
言語
言語 eng
著者 M Yamamoto

× M Yamamoto

en M Yamamoto

Search repository
H Kawakatsu

× H Kawakatsu

en H Kawakatsu

Search repository
K Yomogida

× K Yomogida

en K Yomogida

Search repository
J Koyama

× J Koyama

en J Koyama

Search repository
抄録
内容記述タイプ Other
内容記述 [1] From a temporal deployment of a broadband seismic network at Usu volcano, Japan, we observed long-period (12 sec) volcanic tremors during the first few weeks of the eruptive activity which started in the end of March, 2000. The source of these long period tremors are located relatively deep at a depth of 5 km, and their amplitude variation well correlates with the uplift rate of the eruption area. We thus attribute these long period tremors to the flow induced vibration of a magma chamber and its outlet located around the source region of the long period tremors. This may be the first seismological detection of long-period (> 10 sec) vibrations of a deep magma plumbing system.
言語 en
書誌情報 en : GEOPHYSICAL RESEARCH LETTERS

巻 29, 号 9, p. 1329
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 1944-8007
DOI
関連識別子 10.1029/2001GL013996
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:54:10.741863
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