WEKO3
アイテム
{"_buckets": {"deposit": "37a11fa8-1c15-4630-83e0-b71b48e33058"}, "_deposit": {"created_by": 4, "id": "6073", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "6073"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00006073", "sets": ["782"]}, "author_link": ["9961"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2005-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "212", "bibliographicPageStart": "202", "bibliographicVolumeNumber": "18", "bibliographic_titles": [{"bibliographic_title": "Antarctic meteorite research"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Ikeda, Yukio", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "9961", "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": "Unusual inclusions occur within olivine megacrysts in the DaG735 olivine-phyric shergottite. They consist of pyroxene and chromite in a ratio of about 2:1, and show strange textures. They are grouped into two types, symplectic and non-symplectic. The pyroxenes in unusual inclusions are similar in composition to those in the main lithology of DaG735, but the chromites differ in TiO_2 contents which are lower by half than those of chromites in the main lithology. The symplectic textures indicate exsolution origin of the unusual inclusions within olivine megacrysts, and the reaction to produce the unusual inclusions suggests that the original olivine megacrysts may have contained some amounts of Cr^(+2) in addition to Cr^(+3), and the Cr^(+2) was oxidized to Cr^(+3) during the formation of the unusual inclusions.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00006073", "subitem_identifier_reg_type": "JaLC"}]}, "item_1_publisher_22": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "National Institute of Polar Research"}]}, "item_1_source_id_13": {"attribute_name": "雑誌書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AA11182426", "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 Materials and Biological Sciences, Ibaraki University"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2005-03-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00002499479.pdf", "filesize": [{"value": "1.9 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1900000.0, "url": {"label": "KJ00002499479", "url": "https://nipr.repo.nii.ac.jp/record/6073/files/KJ00002499479.pdf"}, "version_id": "cb3f42b2-78f8-4a0d-a630-04d7da2d85e2"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "martian meteorites, olivine-phyric shergottites, DaG735, inclusions in olivine, chromite", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}]}, "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": "Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite"}]}, "item_type_id": "1", "owner": "4", "path": ["782"], "permalink_uri": "https://doi.org/10.15094/00006073", "pubdate": {"attribute_name": "公開日", "attribute_value": "2005-03-01"}, "publish_date": "2005-03-01", "publish_status": "0", "recid": "6073", "relation": {}, "relation_version_is_last": true, "title": ["Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite"], "weko_shared_id": 4}
Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite
https://doi.org/10.15094/00006073
https://doi.org/10.15094/0000607344f58336-026b-4544-b1f9-3afa32330cb2
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002499479 (1.9 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2005-03-01 | |||||
タイトル | ||||||
タイトル | Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | martian meteorites, olivine-phyric shergottites, DaG735, inclusions in olivine, chromite | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00006073 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | Unusual inclusions within olivine megacrysts in the Dar al Gani 735 shergottite | |||||
著者名(英) |
Ikeda, Yukio
× Ikeda, Yukio |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Materials and Biological Sciences, Ibaraki University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Unusual inclusions occur within olivine megacrysts in the DaG735 olivine-phyric shergottite. They consist of pyroxene and chromite in a ratio of about 2:1, and show strange textures. They are grouped into two types, symplectic and non-symplectic. The pyroxenes in unusual inclusions are similar in composition to those in the main lithology of DaG735, but the chromites differ in TiO_2 contents which are lower by half than those of chromites in the main lithology. The symplectic textures indicate exsolution origin of the unusual inclusions within olivine megacrysts, and the reaction to produce the unusual inclusions suggests that the original olivine megacrysts may have contained some amounts of Cr^(+2) in addition to Cr^(+3), and the Cr^(+2) was oxidized to Cr^(+3) during the formation of the unusual inclusions. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11182426 | |||||
書誌情報 |
Antarctic meteorite research 巻 18, p. 202-212, 発行日 2005-03 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |