WEKO3
アイテム
{"_buckets": {"deposit": "297751ea-2449-491e-a1ec-772baf43b2b1"}, "_deposit": {"created_by": 4, "id": "4582", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "4582"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00004582", "sets": ["589"]}, "author_link": ["9865", "57951"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1992-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "269", "bibliographicPageStart": "258", "bibliographicVolumeNumber": "5", "bibliographic_titles": [{"bibliographic_title": "Proceedings of the NIPR Symposium on Antarctic Meteorites"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Fujita, Takashi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "9865", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kitamura, Masao", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "57951", "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": "A troilite-rich clast enclosing chondrules was found in the Moorabie chondrite (L3). This chondrite is characterized by elongate morphology of chondrules produced by shock deformation. Average composition of the metal and troilite grains in the clast is close to the eutectic composition of the Fe-S system, indicating the melting origin of the clast. The eutectic composition provides the heating temperature to be around 1000℃. Size and distribution of troilite and metal grains in the clast suggest the slow cooling after the melting. Pentlandite as an exsolved phase of troilite in the clast, found first in ordinary chondrites, also supports the melting and slow cooling. Thermal history of the clast indicates that the melting of the opaque minerals and the elongate morphology of chondrules were caused inside the parent body by the shock event which occurred at an early hot stage (around 400℃) of the cooling after the accretion of the chondrite.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00004582", "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": "AA10784627", "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, KyotoUniversity"}, {"subitem_text_language": "en", "subitem_text_value": "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": "1992-03-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000036388.pdf", "filesize": [{"value": "1.3 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1300000.0, "url": {"label": "KJ00000036388", "url": "https://nipr.repo.nii.ac.jp/record/4582/files/KJ00000036388.pdf"}, "version_id": "4e82f864-d54b-4a30-b89e-2dbfa725517b"}]}, "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": "Shock melting origin of a troilite-rich clast in the Moorabiechondrite (L3)", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Shock melting origin of a troilite-rich clast in the Moorabiechondrite (L3)"}]}, "item_type_id": "1", "owner": "4", "path": ["589"], "permalink_uri": "https://doi.org/10.15094/00004582", "pubdate": {"attribute_name": "公開日", "attribute_value": "1992-03-01"}, "publish_date": "1992-03-01", "publish_status": "0", "recid": "4582", "relation": {}, "relation_version_is_last": true, "title": ["Shock melting origin of a troilite-rich clast in the Moorabiechondrite (L3)"], "weko_shared_id": 4}
Shock melting origin of a troilite-rich clast in the Moorabiechondrite (L3)
https://doi.org/10.15094/00004582
https://doi.org/10.15094/0000458298219792-547b-4a58-93c1-54735e37bcbe
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000036388 (1.3 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1992-03-01 | |||||
タイトル | ||||||
タイトル | Shock melting origin of a troilite-rich clast in the Moorabiechondrite (L3) | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00004582 | |||||
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) | |||||
著者名(英) |
Fujita, Takashi
× Fujita, Takashi× Kitamura, Masao |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy,Faculty of Science, KyotoUniversity | ||||||
著者所属(英) | ||||||
en | ||||||
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 | A troilite-rich clast enclosing chondrules was found in the Moorabie chondrite (L3). This chondrite is characterized by elongate morphology of chondrules produced by shock deformation. Average composition of the metal and troilite grains in the clast is close to the eutectic composition of the Fe-S system, indicating the melting origin of the clast. The eutectic composition provides the heating temperature to be around 1000℃. Size and distribution of troilite and metal grains in the clast suggest the slow cooling after the melting. Pentlandite as an exsolved phase of troilite in the clast, found first in ordinary chondrites, also supports the melting and slow cooling. Thermal history of the clast indicates that the melting of the opaque minerals and the elongate morphology of chondrules were caused inside the parent body by the shock event which occurred at an early hot stage (around 400℃) of the cooling after the accretion of the chondrite. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10784627 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Meteorites 巻 5, p. 258-269, 発行日 1992-03 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |