{"_buckets": {"deposit": "62a62e5c-9429-4dd0-930c-ac7bad9fba5b"}, "_deposit": {"id": "18419", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "18419"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00018419"}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2011", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "29", "bibliographicPageStart": "1", "bibliographicVolumeNumber": "58", "bibliographic_titles": [{"bibliographic_title": "The Journal of Earth and Planetary Sciences, Nagoya University"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "A spessartite dyke that intruded into the Permian Kinshozan limestone formed endoskarn that is rich in melanite, along with clinopyroxene and apatite, in a matrix of secondary calcite, thomsonite, stilbite, heulandite and apophyllite. Garnet grains, ranging in size from 0.5 to 3 mm, have dark brown cores and pale to colorless mantles. Detailed analysis of a typical grain reveals TiO2 contents from 2.70 to 11.90 wt.% in the core and from 0.42 to 2.25 wt.% in the mantle. Cation proportions can be attributed to a melanite chemistry controlled by two kinds of substitutions, Ti^4+(Z)=Si(Z) and Fe^2+(Y)Ti^4+(Y)=2^M3+(Y). Iron occurs in both ferric and ferrous states, with Ti substitutions negatively correlated with intermediate to high Fe^3+/(Fe^3++Al). Decreasing ferrous iron from core to mantle is consistent with reverse Mg/(Mg+Fe^2+) zoning in co-genetic clinopyroxene. Low fO2, conditions probably enhanced Fe^2+(Y)Ti^4+(Y)=2M^3+(Y) substitution in garnet.", "subitem_description_type": "Abstract"}]}, "item_9_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/20536"}]}, "item_9_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.18999/joueps.58.1", "subitem_identifier_reg_type": "JaLC"}]}, "item_9_publisher_32": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "Dept. of Earth and Planetary Sciences, Nagoya University"}]}, "item_9_select_15": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_9_source_id_7": {"attribute_name": "ISSN\uff08print\uff09", "attribute_value_mlt": [{"subitem_source_identifier": "0919-875X", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "SUZUKI, Kazuhiro"}], "nameIdentifiers": [{"nameIdentifier": "53509", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "DUNKLEY, Daniel J."}], "nameIdentifiers": [{"nameIdentifier": "53510", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "KAJIZUKA, Izumi"}], "nameIdentifiers": [{"nameIdentifier": "53511", "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": "2018-02-21"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "v58.pdf", "filesize": [{"value": "4.7 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 4700000.0, "url": {"label": "v58.pdf", "url": "https://nagoya.repo.nii.ac.jp/record/18419/files/v58.pdf"}, "version_id": "b3912fde-fae8-47f8-a215-cbe909da7018"}]}, "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": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Melanite from the endoskarn of a spessartite dyke intruding into the Kinshozan limestone in Ogaki City, Gifu Prefecture", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Melanite from the endoskarn of a spessartite dyke intruding into the Kinshozan limestone in Ogaki City, Gifu Prefecture"}]}, "item_type_id": "9", "owner": "1", "path": ["336/337/338/1634"], "permalink_uri": "https://doi.org/10.18999/joueps.58.1", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_value": "2014-09-02"}, "publish_date": "2014-09-02", "publish_status": "0", "recid": "18419", "relation": {}, "relation_version_is_last": true, "title": ["Melanite from the endoskarn of a spessartite dyke intruding into the Kinshozan limestone in Ogaki City, Gifu Prefecture"], "weko_shared_id": null}