{"_buckets": {"deposit": "3c198214-2923-4154-b9d3-04aca7b5ecbb"}, "_deposit": {"id": "10676", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "10676"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00010676"}, "item_12_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1986-03-25", "bibliographicIssueDateType": "Issued"}, "bibliographic_titles": [{}]}]}, "item_12_date_granted_64": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u5e74\u6708\u65e5", "attribute_value_mlt": [{"subitem_dategranted": "1986-03-25"}]}, "item_12_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The buckling phenomena of the subducting lithosphere due\nto the sphericity or the earth are studied by a nonlinear\nfinite element method, and the results are compared with the\nbuckling experiments by Yamaoka et a1. (1986b). The\nsubduction or the lithosphere is modeled by a hemispherical\nshell squeezed at its circumferential edge. For simplicity,\ntwo parameters are employed in scaling the subducting\nlithosphere. One is the thickness or the lithosphere and\nthe other is the length or its deformable portion (i.e. , the\nlength of the descending slab). Uniform inward load is\napplied to the free circumferential edge or the deformable\nportion. At the opposite edge (i.e., at the trench),\nbuilt-in boundary condition is imposed; no displacements and\nno rotations are allowed. Investigations are made mainly on\nthe following three subjects: (I) How do the two parameters\ncontrol the wavelength of buckling? The results show that\nshorter waves are associated with thinner and shorter\nshells. The irregularities such as tears or seamounts do\nnot alter the buckling wavelength very much. (2) How do\nshells deform in their postbuckling state. Sharp cusps\npointing outward appear in the postbuckling undulation\nwithout any irregularities in shell property and in applied\nload\uff65The shape or the cuspidal undulation is quite similar\nt.o that of the actual subducting lithosphere. (3) Can\nbuckling take place in the subducting lithospbere under\nlikely conditions in the earth? The examination is made\nwith respect to the buckling load, the shell deflection, and\nthe buckling wavelength. The results strongly suggest that\nthe arcuate shapes of subduction zones are in fact generated\nby buckling or the subducting lithosphere.", "subitem_description_type": "Abstract"}]}, "item_12_description_5": {"attribute_name": "\u5185\u5bb9\u8a18\u8ff0", "attribute_value_mlt": [{"subitem_description": "\u540d\u53e4\u5c4b\u5927\u5b66\u535a\u58eb\u5b66\u4f4d\u8ad6\u6587 \u5b66\u4f4d\u306e\u7a2e\u985e : \u7406\u5b66\u535a\u58eb(\u8ab2\u7a0b) \u5b66\u4f4d\u6388\u4e0e\u5e74\u6708\u65e5 : \u662d\u548c61\u5e743\u670825\u65e5", "subitem_description_type": "Other"}]}, "item_12_dissertation_number_65": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u756a\u53f7", "attribute_value_mlt": [{"subitem_dissertationnumber": "13901\u7532\u7b2c1831\u53f7"}]}, "item_12_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/12518"}]}, "item_12_select_15": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_12_text_14": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}, {"subitem_text_value": "application/pdf"}]}, "item_12_text_63": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u5e74\u5ea6", "attribute_value_mlt": [{"subitem_text_value": "1985"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "\u5c71\u5ca1, \u8015\u6625"}], "nameIdentifiers": [{"nameIdentifier": "32181", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Yamaoka, Koshun"}], "nameIdentifiers": [{"nameIdentifier": "32182", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-20"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "ko1831_abstr.pdf", "filesize": [{"value": "327.9 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 327900.0, "url": {"label": "ko1831_abstr.pdf ", "url": "https://nagoya.repo.nii.ac.jp/record/10676/files/ko1831_abstr.pdf"}, "version_id": "fdb1cb7f-fc3c-46a7-bfbd-d3589abe44bf"}, {"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-20"}], "displaytype": "detail", "download_preview_message": "", "file_order": 1, "filename": "ko1831.pdf", "filesize": [{"value": "2.7 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 2700000.0, "url": {"label": "ko1831.pdf ", "url": "https://nagoya.repo.nii.ac.jp/record/10676/files/ko1831.pdf"}, "version_id": "622af84d-4c0d-4afb-b19f-6e6bff96016a"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "thesis", "resourceuri": "http://purl.org/coar/resource_type/c_46ec"}]}, "item_title": "SPHERICAL SHELL TECTONICS : ON THE BUCKLING OF THE LITHOSPHERE AT SUBDUCTION ZONES \u7403\u6bbb\u30c6\u30af\u30c8\u30cb\u30af\u30b9 : \u30ea\u30bd\u30b9\u30d5\u30a7\u30a2\u306e\u6c88\u307f\u8fbc\u307f\u306b\u304a\u3051\u308b\u5ea7\u5c48\u73fe\u8c61\u306b\u3064\u3044\u3066", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "SPHERICAL SHELL TECTONICS : ON THE BUCKLING OF THE LITHOSPHERE AT SUBDUCTION ZONES \u7403\u6bbb\u30c6\u30af\u30c8\u30cb\u30af\u30b9 : \u30ea\u30bd\u30b9\u30d5\u30a7\u30a2\u306e\u6c88\u307f\u8fbc\u307f\u306b\u304a\u3051\u308b\u5ea7\u5c48\u73fe\u8c61\u306b\u3064\u3044\u3066"}]}, "item_type_id": "12", "owner": "1", "path": ["336/635/636"], "permalink_uri": "http://hdl.handle.net/2237/12518", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_value": "2009-12-22"}, "publish_date": "2009-12-22", "publish_status": "0", "recid": "10676", "relation": {}, "relation_version_is_last": true, "title": ["SPHERICAL SHELL TECTONICS : ON THE BUCKLING OF THE LITHOSPHERE AT SUBDUCTION ZONES \u7403\u6bbb\u30c6\u30af\u30c8\u30cb\u30af\u30b9 : \u30ea\u30bd\u30b9\u30d5\u30a7\u30a2\u306e\u6c88\u307f\u8fbc\u307f\u306b\u304a\u3051\u308b\u5ea7\u5c48\u73fe\u8c61\u306b\u3064\u3044\u3066"], "weko_shared_id": null}