ログイン
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

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": "701c2772-0209-42fb-801d-75a06c9e5711"}, "_deposit": {"id": "27195", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "27195"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00027195", "sets": ["1910"]}, "author_link": ["89122", "89123"], "item_10_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2018-10", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "10", "bibliographicPageEnd": "9285", "bibliographicPageStart": "9269", "bibliographicVolumeNumber": "123", "bibliographic_titles": [{"bibliographic_title": "Journal of Geophysical Research: Solid Earth"}]}]}, "item_10_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "We investigate the evolution of tectonic background stress and elastic as well as inelastic strain in a crust‐upper mantle system around an infinitely long vertical strike‐slip fault in a self‐consistent mechanical earthquake cycle model. In the early stage of the stress evolution, deformation of the crust and the upper mantle is dominated by a uniform simple shear. Shear localization in the lower crust starts when coseismic rupture extends to the entire brittle upper crust. Together with this transition, the earthquake recurrence intervals decrease by an order of magnitude due to a basal drag originated from a localized plastic flow of the lower crust. After the shear zone is fully developed in the lower crust, the fault slip rate catches up with the far‐field velocity and earthquakes starts to occur periodically. Such a steady state can be reached in several hundred thousand years from the beginning, which includes few hundreds of earthquake cycles. A shear zone with large cumulative strain needs a few million years to develop under an intraplate strike‐slip fault, which is much longer than the time for shear strain rate to be localized. The model successfully reproduced evolution of tectonic stress around an intraplate strike‐slip fault, interacting with the development of localized shear zone in the lower crust. The model demonstrates the importance of considering the whole mechanical system in which rheological structure and fault activities interacting with each other for the better understanding of the intraplate earthquakes.", "subitem_description_language": "en", "subitem_description_type": "Abstract"}]}, "item_10_description_5": {"attribute_name": "内容記述", "attribute_value_mlt": [{"subitem_description": "ファイル公開:2019-04-01", "subitem_description_language": "ja", "subitem_description_type": "Other"}]}, "item_10_publisher_32": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "Wiley", "subitem_publisher_language": "en"}]}, "item_10_relation_11": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type": "isVersionOf", "subitem_relation_type_id": {"subitem_relation_type_id_text": "https://doi.org/10.1029/2018JB016421", "subitem_relation_type_select": "DOI"}}]}, "item_10_rights_12": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "© 2018 American Geophysical Union", "subitem_rights_language": "en"}]}, "item_10_select_15": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_10_source_id_61": {"attribute_name": "ISSN(print)", "attribute_value_mlt": [{"subitem_source_identifier": "2169-9313", "subitem_source_identifier_type": "PISSN"}]}, "item_10_source_id_62": {"attribute_name": "ISSN(Online)", "attribute_value_mlt": [{"subitem_source_identifier": "2169-9356", "subitem_source_identifier_type": "EISSN"}]}, "item_1615787544753": {"attribute_name": "出版タイプ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_access_right": {"attribute_name": "アクセス権", "attribute_value_mlt": [{"subitem_access_right": "open access", "subitem_access_right_uri": "http://purl.org/coar/access_right/c_abf2"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Zhang, Xuelei", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "89122", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Sagiya, Takeshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "89123", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2019-04-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "Zhang_et_al-2018-Journal_of_Geophysical_Research__Solid_Earth.pdf", "filesize": [{"value": "2.8 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 2800000.0, "url": {"label": "Zhang_et_al-2018-Journal_of_Geophysical_Research__Solid_Earth", "objectType": "fulltext", "url": "https://nagoya.repo.nii.ac.jp/record/27195/files/Zhang_et_al-2018-Journal_of_Geophysical_Research__Solid_Earth.pdf"}, "version_id": "3afc5e6f-d423-496c-a328-e67cebf37881"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "earthquake cycle", "subitem_subject_scheme": "Other"}, {"subitem_subject": "nonlinear Maxwell rheology", "subitem_subject_scheme": "Other"}, {"subitem_subject": "plastic shear zone evolution", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Intraplate Strike-Slip Faulting, Stress Accumulation, and Shear Localization of a Crust-Upper Mantle System With Nonlinear Viscoelastic Material", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Intraplate Strike-Slip Faulting, Stress Accumulation, and Shear Localization of a Crust-Upper Mantle System With Nonlinear Viscoelastic Material", "subitem_title_language": "en"}]}, "item_type_id": "10", "owner": "1", "path": ["1910"], "permalink_uri": "http://hdl.handle.net/2237/00029394", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2019-03-06"}, "publish_date": "2019-03-06", "publish_status": "0", "recid": "27195", "relation": {}, "relation_version_is_last": true, "title": ["Intraplate Strike-Slip Faulting, Stress Accumulation, and Shear Localization of a Crust-Upper Mantle System With Nonlinear Viscoelastic Material"], "weko_shared_id": -1}
  1. H210 減災連携研究センター
  2. H210a 雑誌掲載論文
  3. 学術雑誌

Intraplate Strike-Slip Faulting, Stress Accumulation, and Shear Localization of a Crust-Upper Mantle System With Nonlinear Viscoelastic Material

http://hdl.handle.net/2237/00029394
http://hdl.handle.net/2237/00029394
e88ce6c5-540b-4685-a4e2-06937f50e93a
名前 / ファイル ライセンス アクション
Zhang_et_al-2018-Journal_of_Geophysical_Research__Solid_Earth.pdf Zhang_et_al-2018-Journal_of_Geophysical_Research__Solid_Earth (2.8 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2019-03-06
タイトル
タイトル Intraplate Strike-Slip Faulting, Stress Accumulation, and Shear Localization of a Crust-Upper Mantle System With Nonlinear Viscoelastic Material
言語 en
著者 Zhang, Xuelei

× Zhang, Xuelei

WEKO 89122

en Zhang, Xuelei

Search repository
Sagiya, Takeshi

× Sagiya, Takeshi

WEKO 89123

en Sagiya, Takeshi

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
言語 en
権利情報 © 2018 American Geophysical Union
キーワード
主題Scheme Other
主題 earthquake cycle
キーワード
主題Scheme Other
主題 nonlinear Maxwell rheology
キーワード
主題Scheme Other
主題 plastic shear zone evolution
抄録
内容記述 We investigate the evolution of tectonic background stress and elastic as well as inelastic strain in a crust‐upper mantle system around an infinitely long vertical strike‐slip fault in a self‐consistent mechanical earthquake cycle model. In the early stage of the stress evolution, deformation of the crust and the upper mantle is dominated by a uniform simple shear. Shear localization in the lower crust starts when coseismic rupture extends to the entire brittle upper crust. Together with this transition, the earthquake recurrence intervals decrease by an order of magnitude due to a basal drag originated from a localized plastic flow of the lower crust. After the shear zone is fully developed in the lower crust, the fault slip rate catches up with the far‐field velocity and earthquakes starts to occur periodically. Such a steady state can be reached in several hundred thousand years from the beginning, which includes few hundreds of earthquake cycles. A shear zone with large cumulative strain needs a few million years to develop under an intraplate strike‐slip fault, which is much longer than the time for shear strain rate to be localized. The model successfully reproduced evolution of tectonic stress around an intraplate strike‐slip fault, interacting with the development of localized shear zone in the lower crust. The model demonstrates the importance of considering the whole mechanical system in which rheological structure and fault activities interacting with each other for the better understanding of the intraplate earthquakes.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 ファイル公開:2019-04-01
言語 ja
内容記述タイプ Other
出版者
言語 en
出版者 Wiley
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1029/2018JB016421
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 2169-9313
ISSN(Online)
収録物識別子タイプ EISSN
収録物識別子 2169-9356
書誌情報 Journal of Geophysical Research: Solid Earth

巻 123, 号 10, p. 9269-9285, 発行日 2018-10
著者版フラグ
値 publisher
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 10:41:37.641807
Show All versions

Share

Mendeley Twitter Facebook Print Addthis

Cite as

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


Powered by WEKO3