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": "65486a81-93d5-4e40-b0ed-619f214777f0"}, "_deposit": {"id": "6857", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "6857"}, "status": "published"}, "_oai": {"id": "oai:niigata-u.repo.nii.ac.jp:00006857", "sets": ["456", "194"]}, "item_7_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2005-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "99", "bibliographicPageStart": "47", "bibliographicVolumeNumber": "20", "bibliographic_titles": [{"bibliographic_title": "Science reports of Niigata University. (Geology)"}, {"bibliographic_title": "Science reports of Niigata University. (Geology)", "bibliographic_titleLang": "en"}]}]}, "item_7_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The present study was performed to examine the detailed exhumation process of deepsheeted materials in accretionary complexes by analysis of deformed minorstructures recorded in a low-grade schist zone, reconstructed by tracing sporadically distributed lowgrade schist bodies with similar constituent rocks, metamorphism, and deformation history in the Joetsu Belt and the Western Zone of the Ashio Belt belonging to the Paleozoic to Mesozoic systems of the Inner Zone of Southwest Japan. Geometric and kinematic analyses of deformed minor- and microstructures divided the whole deformation process into two deformation phases, i.e., the earlier deformation phase (phase 1 deformation) showing a sinistral shear regime with the deformation mechanism of crystal plasticity and diffusive mass transfer, and the later deformation phase (phase 2 deformation) showing a dextral shear regime with the deformation mechanism of fracture, slip, and cataclasis. Deformation facies analysis showed the temporal and spatial sequences (deformation zoning) of the deformed minorstructures. The former showed that deformed minorstructures formed under conditions of decreasing mean ductility with time in response to rock body exhumation, and the latter showed that mean ductility represented by the assemblage of deformed minorstructures decreased with distance from the axial part of a major isoclinal syncline in the western limb. The two inverted shear regimes were caused by alternate movement of oceanic and continental plates, i.e., NE-directed oblique subduction of the oceanic plate and NE-ENE-directed oblique upthrusting being reactivation of the Hida Nappe belonging to the continental plate. The mutual movements of the two plates played an important role in the development of the accretionary complex of the Japanese Islands.", "subitem_description_type": "Abstract"}]}, "item_7_publisher_7": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "新潟大学理学部"}]}, "item_7_select_19": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_7_source_id_11": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AA11436808", "subitem_source_identifier_type": "NCID"}]}, "item_7_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "13491237", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Takenouchi, Ko"}], "nameIdentifiers": [{"nameIdentifier": "54459", "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": "2019-08-06"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "20_47-99.pdf", "filesize": [{"value": "28.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 28100000.0, "url": {"label": "20_47-99.pdf", "url": "https://niigata-u.repo.nii.ac.jp/record/6857/files/20_47-99.pdf"}, "version_id": "230a68da-bce1-4525-b745-1ebfd4cf3dfd"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "accretionary complex", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Ashio Belt", "subitem_subject_scheme": "Other"}, {"subitem_subject": "deformation facies analysis", "subitem_subject_scheme": "Other"}, {"subitem_subject": "exhumation process", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Joetsu Belt", "subitem_subject_scheme": "Other"}, {"subitem_subject": "low-grade schist", "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": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan"}, {"subitem_title": "Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan", "subitem_title_language": "en"}]}, "item_type_id": "7", "owner": "1", "path": ["456", "194"], "permalink_uri": "http://hdl.handle.net/10191/2129", "pubdate": {"attribute_name": "公開日", "attribute_value": "2017-09-04"}, "publish_date": "2017-09-04", "publish_status": "0", "recid": "6857", "relation": {}, "relation_version_is_last": true, "title": ["Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan"], "weko_shared_id": null}
  1. 050 理学部
  2. 20 紀要
  3. 02 Science reports of Niigata University. (Geology)
  4. No.20
  1. 0 資料タイプ別
  2. 03 紀要論文

Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan

http://hdl.handle.net/10191/2129
http://hdl.handle.net/10191/2129
08c91419-2b63-4827-9c1d-3db0e02f398a
名前 / ファイル ライセンス アクション
20_47-99.pdf 20_47-99.pdf (28.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2017-09-04
タイトル
タイトル Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan
タイトル
言語 en
タイトル Deformation facies analysis and tectonic evolution of low-grade schists in the Joetsu region, central Japan
言語
言語 eng
キーワード
主題Scheme Other
主題 accretionary complex
キーワード
主題Scheme Other
主題 Ashio Belt
キーワード
主題Scheme Other
主題 deformation facies analysis
キーワード
主題Scheme Other
主題 exhumation process
キーワード
主題Scheme Other
主題 Joetsu Belt
キーワード
主題Scheme Other
主題 low-grade schist
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 Takenouchi, Ko

× Takenouchi, Ko

WEKO 54459

Takenouchi, Ko

Search repository
抄録
内容記述タイプ Abstract
内容記述 The present study was performed to examine the detailed exhumation process of deepsheeted materials in accretionary complexes by analysis of deformed minorstructures recorded in a low-grade schist zone, reconstructed by tracing sporadically distributed lowgrade schist bodies with similar constituent rocks, metamorphism, and deformation history in the Joetsu Belt and the Western Zone of the Ashio Belt belonging to the Paleozoic to Mesozoic systems of the Inner Zone of Southwest Japan. Geometric and kinematic analyses of deformed minor- and microstructures divided the whole deformation process into two deformation phases, i.e., the earlier deformation phase (phase 1 deformation) showing a sinistral shear regime with the deformation mechanism of crystal plasticity and diffusive mass transfer, and the later deformation phase (phase 2 deformation) showing a dextral shear regime with the deformation mechanism of fracture, slip, and cataclasis. Deformation facies analysis showed the temporal and spatial sequences (deformation zoning) of the deformed minorstructures. The former showed that deformed minorstructures formed under conditions of decreasing mean ductility with time in response to rock body exhumation, and the latter showed that mean ductility represented by the assemblage of deformed minorstructures decreased with distance from the axial part of a major isoclinal syncline in the western limb. The two inverted shear regimes were caused by alternate movement of oceanic and continental plates, i.e., NE-directed oblique subduction of the oceanic plate and NE-ENE-directed oblique upthrusting being reactivation of the Hida Nappe belonging to the continental plate. The mutual movements of the two plates played an important role in the development of the accretionary complex of the Japanese Islands.
書誌情報 Science reports of Niigata University. (Geology)
en : Science reports of Niigata University. (Geology)

巻 20, p. 47-99, 発行日 2005-03
出版者
出版者 新潟大学理学部
ISSN
収録物識別子タイプ ISSN
収録物識別子 13491237
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA11436808
著者版フラグ
値 publisher
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 19:28:44.266973
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