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": "ca366637-48be-4aec-8560-ae0b8d56d78e"}, "_deposit": {"id": "2866", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "2866"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00002866", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2019-03", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "3", "bibliographicPageEnd": "3023", "bibliographicPageStart": "3011", "bibliographicVolumeNumber": "124", "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": "We investigate seismic velocity changes in response to the tidal strain at Izu-Oshima volcano, Japan, by analyzing the data of permanent seismic stations and a small seismic array to evaluate the characteristics of strain sensitivity of velocity changes. We estimate the seismic velocity changes by phase differences between cross-correlations functions of ambient noises at the frequency of 2-4Hz stacked for time periods with different tidal strain amplitudes. The seismic velocity changes decrease and increase during dilatation and contraction periods, respectively, when analyzing the cross-correlations functions at early lapse times ranging from 2 to 7s. The strain sensitivity of seismic velocity changes is estimated to be x104 at the early lapse times. However, we find that strain sensitivity of the seismic velocity changes decreases when analyzing the cross-correlation functions at later lapse times from 7s to 35s. Applying an array analysis to the cross-correlation functions, we observe apparent velocities of about 1km/s at the early lapse times and those of higher than 1km/s at the late lapse times. Since the group velocity of Rayleigh waves is 1.1km/s at Izu-Oshima volcano, the apparent velocities at the late lapse times may indicate the scattered or reflected body waves incident from a deeper region. Decrease of strain sensitivity with the lapse times therefore results from the emergence of body waves on the late lapse times. These results highlight the need to pay attention to wave types of cross-correlation functions and their paths to interpret seismic velocity changes.", "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": "10.1029/2018JB016235"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "2169-9356", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Tomoya Takano", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Takeshi Nishimura", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hisashi Nakahara", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hideki Ueda", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Eisuke Fujita", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Sensitivity of Seismic Velocity Changes to the Tidal Strain at Different Lapse Times: Data Analyses of a Small Seismic Array at Izu-Oshima Volcano", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Sensitivity of Seismic Velocity Changes to the Tidal Strain at Different Lapse Times: Data Analyses of a Small Seismic Array at Izu-Oshima Volcano", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/2866", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "2866", "relation": {}, "relation_version_is_last": true, "title": ["Sensitivity of Seismic Velocity Changes to the Tidal Strain at Different Lapse Times: Data Analyses of a Small Seismic Array at Izu-Oshima Volcano"], "weko_shared_id": -1}
  1. 防災科研関係論文

Sensitivity of Seismic Velocity Changes to the Tidal Strain at Different Lapse Times: Data Analyses of a Small Seismic Array at Izu-Oshima Volcano

https://nied-repo.bosai.go.jp/records/2866
https://nied-repo.bosai.go.jp/records/2866
59bb8174-98c3-4461-bea2-70b90853cdeb
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Sensitivity of Seismic Velocity Changes to the Tidal Strain at Different Lapse Times: Data Analyses of a Small Seismic Array at Izu-Oshima Volcano
言語
言語 eng
著者 Tomoya Takano

× Tomoya Takano

en Tomoya Takano

Search repository
Takeshi Nishimura

× Takeshi Nishimura

en Takeshi Nishimura

Search repository
Hisashi Nakahara

× Hisashi Nakahara

en Hisashi Nakahara

Search repository
Hideki Ueda

× Hideki Ueda

en Hideki Ueda

Search repository
Eisuke Fujita

× Eisuke Fujita

en Eisuke Fujita

Search repository
抄録
内容記述タイプ Other
内容記述 We investigate seismic velocity changes in response to the tidal strain at Izu-Oshima volcano, Japan, by analyzing the data of permanent seismic stations and a small seismic array to evaluate the characteristics of strain sensitivity of velocity changes. We estimate the seismic velocity changes by phase differences between cross-correlations functions of ambient noises at the frequency of 2-4Hz stacked for time periods with different tidal strain amplitudes. The seismic velocity changes decrease and increase during dilatation and contraction periods, respectively, when analyzing the cross-correlations functions at early lapse times ranging from 2 to 7s. The strain sensitivity of seismic velocity changes is estimated to be x104 at the early lapse times. However, we find that strain sensitivity of the seismic velocity changes decreases when analyzing the cross-correlation functions at later lapse times from 7s to 35s. Applying an array analysis to the cross-correlation functions, we observe apparent velocities of about 1km/s at the early lapse times and those of higher than 1km/s at the late lapse times. Since the group velocity of Rayleigh waves is 1.1km/s at Izu-Oshima volcano, the apparent velocities at the late lapse times may indicate the scattered or reflected body waves incident from a deeper region. Decrease of strain sensitivity with the lapse times therefore results from the emergence of body waves on the late lapse times. These results highlight the need to pay attention to wave types of cross-correlation functions and their paths to interpret seismic velocity changes.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

巻 124, 号 3, p. 3011-3023, 発行日 2019-03
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 2169-9356
DOI
関連識別子 10.1029/2018JB016235
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-30 09:19:58.323951
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