{"_buckets": {"deposit": "b7cbf404-7c9d-4100-a333-e937a35de9ce"}, "_deposit": {"id": "18425", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "18425"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00018425"}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2013", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "110", "bibliographicPageStart": "101", "bibliographicVolumeNumber": "60", "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": "We have measured the Ca and REE compositions of seven kimuraite samples, which are subsamples taken from a spherulitic aggregate kimuraite sample filling a void in the alkali olivine basalt. In the chondrite-normalized REE patterns, all samples yielded parallel concave tetrad patterns, and the mole ratios of \u03a3(REE+ Y) to Ca were calculated to be 2.5 to 3.4, all of which were obviously larger than the ideal value 2.0 of kimuraite. In addition, electron-probe microanalyzer (EPMA) was also applied to determine the compositions of our samples. Though only four rare earth elements (Y, La, Pr and Nd) were able to be measured, the mole ratios of \u03a3(REE+ Y) to Ca of thirty-two point analyses determined with EPMA were 2.1 to 3.3. Both analytical results demonstrated that our kimuraite samples might have excessive amount of REE. In the backscattered electron (BSE) images, besides dark kimuraite grains, the presence of another mineral with brighter BSE intensity along the cleavages of kimuraite grains was confirmed, and almost all analysis spots of EPMA failed to escape from the contamination of this mineral. The most possible candidate for this mineral is lanthanite, both for its close association with kimuraite and for its characteristic chemical composition. The compositions of our kimuraite samples, especially LREE, have been modified due to the presence of a small portion of lanthanite, but the concave tetrad pattern remains, as lanthanite seems to have a similar concave tetrad pattern like kimuraite.", "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/2237/20542"}]}, "item_9_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.18999/joueps.60.101", "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": "JIAO, Wenfang"}], "nameIdentifiers": [{"nameIdentifier": "53525", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "KAWABE, Iwao"}], "nameIdentifiers": [{"nameIdentifier": "53526", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "KATO, Takenori"}], "nameIdentifiers": [{"nameIdentifier": "53527", "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": "60-3.pdf", "filesize": [{"value": "1.2 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 1200000.0, "url": {"label": "60-3.pdf", "url": "https://nagoya.repo.nii.ac.jp/record/18425/files/60-3.pdf"}, "version_id": "34c0df30-6a04-4bd0-a097-0f3586c99217"}]}, "item_keyword": {"attribute_name": "\u30ad\u30fc\u30ef\u30fc\u30c9", "attribute_value_mlt": [{"subitem_subject": "rare earth elements", "subitem_subject_scheme": "Other"}, {"subitem_subject": "kimuraite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "lanthanite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "tetrad effect", "subitem_subject_scheme": "Other"}]}, "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": "Reexamination of kimuraite : the occurrence of lanthanite in the cleavages of kimuraite", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Reexamination of kimuraite : the occurrence of lanthanite in the cleavages of kimuraite"}]}, "item_type_id": "9", "owner": "1", "path": ["336/337/338/1636"], "permalink_uri": "https://doi.org/10.18999/joueps.60.101", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_value": "2014-09-02"}, "publish_date": "2014-09-02", "publish_status": "0", "recid": "18425", "relation": {}, "relation_version_is_last": true, "title": ["Reexamination of kimuraite : the occurrence of lanthanite in the cleavages of kimuraite"], "weko_shared_id": null}