{"created":"2022-01-27T02:28:17.200684+00:00","id":2002441,"links":{},"metadata":{"_buckets":{"deposit":"6f188466-0231-4455-9109-728b83f18290"},"_deposit":{"id":"2002441","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"2002441"},"status":"published"},"_oai":{"id":"oai:u-ryukyu.repo.nii.ac.jp:02002441","sets":["1642838163960:1642838338003","1642838403551:1642838406414"]},"author_link":[],"item_1617186331708":{"attribute_name":"Title","attribute_value_mlt":[{"subitem_1551255647225":"SIMULATION OF HIMALAYAN MAJOR THRUSTS BY FINITE ELEMENT METHOD","subitem_1551255648112":"en"},{"subitem_1551255647225":"有限要素法によるヒマラヤの主要スラストのシミュレーション","subitem_1551255648112":"ja"}]},"item_1617186419668":{"attribute_name":"Creator","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Howladar, M. Farhad","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Hayashi, Daigoro","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"林, 大五郎","creatorNameLang":"ja"}]}]},"item_1617186476635":{"attribute_name":"Access Rights","attribute_value_mlt":[{"subitem_1522299639480":"open access","subitem_1600958577026":"http://purl.org/coar/access_right/c_abf2"}]},"item_1617186609386":{"attribute_name":"Subject","attribute_value_mlt":[{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Himalaya"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Finite element method"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Major thrust"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Incipient zone"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"MCT"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"MBT"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"MFT"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"ヒマラヤ"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"有限要素法"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"主要スラスト"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"萌芽地帯"}]},"item_1617186626617":{"attribute_name":"Description","attribute_value_mlt":[{"subitem_description":"The Himalayan mountain system developed from the powerful earth movements which occurred as the Indian plate pressed against the Eurasian continental plate. A series of elastic finite element models are presented to examine the development of major thrusts (MCT, MBT and MFT) in the central Himalaya. Balanced geologic profiles of the central Himalaya which are modified from Johnson's profiles (2002) are used for the purpose under plane strain condition. The convergent rate of India has changed 10 cm/a at 40 Ma, 5 cm/a at 20 Ma and 2 cm/a at 10 Ma. Results show that the horizontal compressive stress σ_1 leads to the development of thrust faults in the Ththys Himalaya, Higher Himalaya, Lesser Himalaya, Sub-Himalaya and incipient zones of MCT, MBT and MFT. Especially, the thrust faults are highly concentrated within the whole area of the incipient zones, which influenced the formation of MCT, MBT and MFT at their early stage.","subitem_description_type":"Other"},{"subitem_description":"大規模な地殻の運動によって出現したヒマラヤ山系はインドプレートとユーラシア大陸プレートとの衝突によりもたらされた．ここに取り上げた一連の弾性有限要素モデルは中央ヒマラヤの主要スラスト（MCT，MBT，MFT）の発達過程を表している．Johnson（2002）によって作成された中央ヒマラヤのバランス地質断面図を多少修正したものを平面ひずみの条件のもとで使用した．インドプレートの速度を40Maでは10cm／年，20Maでは5cm／年，10Maでは2cm／年に設定した．シミュレーションの結果，水平圧縮応力σ_1はテーチスヒマラヤ，高ヒマラヤ，低ヒマラヤ，サブヒマラヤ，そしてMCT，MBT，MFTの萌芽地帯にスラストを生じさせた．特に将来MCT，MBT，MFTとなる萌芽地帯全体でのスラストの発生する領域の占める割合は高い．","subitem_description_type":"Other"},{"subitem_description":"論文","subitem_description_type":"Other"}]},"item_1617186643794":{"attribute_name":"Publisher","attribute_value_mlt":[{"subitem_1522300295150":"ja","subitem_1522300316516":"日本情報地質学会"}]},"item_1617186702042":{"attribute_name":"Language","attribute_value_mlt":[{"subitem_1551255818386":"eng"}]},"item_1617186783814":{"attribute_name":"Identifier","attribute_value_mlt":[{"subitem_identifier_type":"HDL","subitem_identifier_uri":"http://hdl.handle.net/20.500.12000/2949"}]},"item_1617186920753":{"attribute_name":"Source Identifier","attribute_value_mlt":[{"subitem_1522646500366":"ISSN","subitem_1522646572813":"0388-502X"},{"subitem_1522646500366":"NCID","subitem_1522646572813":"AN0036643X"}]},"item_1617186941041":{"attribute_name":"Source Title","attribute_value_mlt":[{"subitem_1522650068558":"ja","subitem_1522650091861":"情報地質 ＝ Geological data processing (Geoinformatics)"}]},"item_1617187056579":{"attribute_name":"Bibliographic Information","attribute_value_mlt":[{"bibliographicIssueNumber":"4","bibliographicPageEnd":"219","bibliographicPageStart":"207","bibliographicVolumeNumber":"15"}]},"item_1617258105262":{"attribute_name":"Resource Type","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_1617265215918":{"attribute_name":"Version Type","attribute_value_mlt":[{"subitem_1522305645492":"VoR","subitem_1600292170262":"http://purl.org/coar/version/c_970fb48d4fbd8a85"}]},"item_1617605131499":{"attribute_name":"File","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","filename":"Hayashi_d-04.pdf","mimetype":"application/pdf","url":{"objectType":"fulltext","url":"https://u-ryukyu.repo.nii.ac.jp/record/2002441/files/Hayashi_d-04.pdf"},"version_id":"7762dc8d-d8f8-446d-b1a8-e40d70323e43"}]},"item_title":"SIMULATION OF HIMALAYAN MAJOR THRUSTS BY FINITE ELEMENT METHOD","item_type_id":"15","owner":"1","path":["1642838338003","1642838406414"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-01-15"},"publish_date":"2008-01-15","publish_status":"0","recid":"2002441","relation_version_is_last":true,"title":["SIMULATION OF HIMALAYAN MAJOR THRUSTS BY FINITE ELEMENT METHOD"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-08-03T05:25:01.441058+00:00"}