WEKO3
アイテム
{"_buckets": {"deposit": "99cb852e-06f9-49cf-98b4-ec5ab5b44cfd"}, "_deposit": {"created_by": 4, "id": "2125", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "2125"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00002125", "sets": ["400"]}, "author_link": ["57984", "1373", "57983", "57951"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1987-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "122", "bibliographicPageStart": "113", "bibliographicVolumeNumber": "46", "bibliographic_titles": [{"bibliographic_title": "Memoirs of National Institute of Polar Research. Special issue"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Kitamura, Masao", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "57951", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Watanabe, Seiko", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "1373", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Isobe, Hiroshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "57983", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Morimoto, Nobuo", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "57984", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_description_1": {"attribute_name": "ページ属性", "attribute_value_mlt": [{"subitem_description": "P(論文)", "subitem_description_type": "Other"}]}, "item_1_description_12": {"attribute_name": "抄録(英)", "attribute_value_mlt": [{"subitem_description": "Diopside in the chondrules in Y-691 (EH3), most of which include enstatite as phenocrysts, occurs in three different modes; (1) diopside rimming some of the enstatite crystals, (2) single crystals as phenocrysts of the chondrules, and (3) single crystals of diopside enriched in aluminum in one chondrule. The finding of the single crystals of diopside, since that in Qingzhen, indicates their common existence in the E3 chondrites. Common appearance of the single crystals, in contrast with the equilibrated E and the unequilibrated ordinary chondrites, is considered to be related with the reducing condition during the chondrule formation. Crystallization temperature of the crystals is roughly estimated to be 1300-1200℃. Coexistence of aluminum-rich and aluminum-poor diopside in a chondrule implies high pressure episode by shock process.", "subitem_description_type": "Other"}]}, "item_1_source_id_13": {"attribute_name": "雑誌書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AA00733561", "subitem_source_identifier_type": "NCID"}]}, "item_1_text_10": {"attribute_name": "著者所属(英)", "attribute_value_mlt": [{"subitem_text_language": "en", "subitem_text_value": "Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1987-03-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000012678.pdf", "filesize": [{"value": "1.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1100000.0, "url": {"label": "KJ00000012678", "url": "https://nipr.repo.nii.ac.jp/record/2125/files/KJ00000012678.pdf"}, "version_id": "40f77bdb-e342-40a0-ba9f-12ecccd438c4"}]}, "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": "Diopside in chondrules of Yamato-691 (EH3)", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Diopside in chondrules of Yamato-691 (EH3)", "subitem_title_language": "en"}]}, "item_type_id": "1", "owner": "4", "path": ["400"], "permalink_uri": "https://nipr.repo.nii.ac.jp/records/2125", "pubdate": {"attribute_name": "公開日", "attribute_value": "1987-03-01"}, "publish_date": "1987-03-01", "publish_status": "0", "recid": "2125", "relation": {}, "relation_version_is_last": true, "title": ["Diopside in chondrules of Yamato-691 (EH3)"], "weko_shared_id": 4}
Diopside in chondrules of Yamato-691 (EH3)
https://nipr.repo.nii.ac.jp/records/2125
https://nipr.repo.nii.ac.jp/records/21259c492d89-88c5-4aa6-b7a2-5db829d5a99c
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012678 (1.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1987-03-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Diopside in chondrules of Yamato-691 (EH3) | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Kitamura, Masao
× Kitamura, Masao× Watanabe, Seiko× Isobe, Hiroshi× Morimoto, Nobuo |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University/Department of Geology and Mineralogy, Faculty of Science, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Diopside in the chondrules in Y-691 (EH3), most of which include enstatite as phenocrysts, occurs in three different modes; (1) diopside rimming some of the enstatite crystals, (2) single crystals as phenocrysts of the chondrules, and (3) single crystals of diopside enriched in aluminum in one chondrule. The finding of the single crystals of diopside, since that in Qingzhen, indicates their common existence in the E3 chondrites. Common appearance of the single crystals, in contrast with the equilibrated E and the unequilibrated ordinary chondrites, is considered to be related with the reducing condition during the chondrule formation. Crystallization temperature of the crystals is roughly estimated to be 1300-1200℃. Coexistence of aluminum-rich and aluminum-poor diopside in a chondrule implies high pressure episode by shock process. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 46, p. 113-122, 発行日 1987-03 |