WEKO3
アイテム
{"_buckets": {"deposit": "a17c7b4c-07ab-4e0a-9741-04a09a0b42a9"}, "_deposit": {"created_by": 4, "id": "5923", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "5923"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00005923", "sets": ["775"]}, "author_link": ["9852"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1998-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "48", "bibliographicPageStart": "32", "bibliographicVolumeNumber": "11", "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": "McCoy, Timothy J.", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "9852", "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 pyroxene-oldhamite clast in the Bustee aubrite contains major enstatite and minor diopside and forsterite as the silicate host, with abundant (\u0026acd;30vol%), included 1-5mm spherules of oldhamite. Within the oldhamite (\u0026acd;5vol% of the oldhamite) are a variety of phases, including osbornite (TiN), titanoan troilite (17.2-25.2wt% Ti), heideite (28.7-29.4wt% Ti), niningerite, daubreelite, forsterite, and Fe metal. This clast represents only the second occurrence of an oldhamite-rich lithology in aubrites. An igneous origin for oldhamite within the Bustee pyroxene-oldhamite clast is suggested by its large size, rounded shapes, presence of included phases formed from multiple, immiscible sulfides, and inclusion of phases unknown from enstatite chondrites. The Bustee clast contains a variety of Ti-rich phases. This work suggests Ti-rich troilite observed in aubrites formed by co-crystallization with or exsolution from Ti-poor sulfides (e.g., oldhamite). In the Bustee case, the undetectably low Ti concentrations in oldhamite and experimental Ti partition coefficient between FeS and CaS approaching infinity support such a suggestion. This mechanism solves the long-standing problem of enriching aubritic troilite in Ti and weakens arguments against a direct derivation of aubrites from known enstatite chondrites.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00005923", "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 Mineral Sciences, MRC 119, National Museum of Natural History, Smithsonian Institution"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1998-03-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000040915.pdf", "filesize": [{"value": "1.7 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1700000.0, "url": {"label": "KJ00000040915", "url": "https://nipr.repo.nii.ac.jp/record/5923/files/KJ00000040915.pdf"}, "version_id": "e858c785-f661-4b28-8273-060242721b71"}]}, "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": "A pyroxene-oldhamite clast in Bustee: Igneous aubritic oldhamite and a mechanism for the Ti enrichment in aubritic troilite", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "A pyroxene-oldhamite clast in Bustee: Igneous aubritic oldhamite and a mechanism for the Ti enrichment in aubritic troilite"}]}, "item_type_id": "1", "owner": "4", "path": ["775"], "permalink_uri": "https://doi.org/10.15094/00005923", "pubdate": {"attribute_name": "公開日", "attribute_value": "1998-03-01"}, "publish_date": "1998-03-01", "publish_status": "0", "recid": "5923", "relation": {}, "relation_version_is_last": true, "title": ["A pyroxene-oldhamite clast in Bustee: Igneous aubritic oldhamite and a mechanism for the Ti enrichment in aubritic troilite"], "weko_shared_id": 4}
A pyroxene-oldhamite clast in Bustee: Igneous aubritic oldhamite and a mechanism for the Ti enrichment in aubritic troilite
https://doi.org/10.15094/00005923
https://doi.org/10.15094/000059234ce8f9d2-6877-4baa-a4a7-d67896907794
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000040915 (1.7 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1998-03-01 | |||||
タイトル | ||||||
タイトル | A pyroxene-oldhamite clast in Bustee: Igneous aubritic oldhamite and a mechanism for the Ti enrichment in aubritic troilite | |||||
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 | 10.15094/00005923 | |||||
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) |
McCoy, Timothy J.
× McCoy, Timothy J. |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Mineral Sciences, MRC 119, National Museum of Natural History, Smithsonian Institution | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A pyroxene-oldhamite clast in the Bustee aubrite contains major enstatite and minor diopside and forsterite as the silicate host, with abundant (∿30vol%), included 1-5mm spherules of oldhamite. Within the oldhamite (∿5vol% of the oldhamite) are a variety of phases, including osbornite (TiN), titanoan troilite (17.2-25.2wt% Ti), heideite (28.7-29.4wt% Ti), niningerite, daubreelite, forsterite, and Fe metal. This clast represents only the second occurrence of an oldhamite-rich lithology in aubrites. An igneous origin for oldhamite within the Bustee pyroxene-oldhamite clast is suggested by its large size, rounded shapes, presence of included phases formed from multiple, immiscible sulfides, and inclusion of phases unknown from enstatite chondrites. The Bustee clast contains a variety of Ti-rich phases. This work suggests Ti-rich troilite observed in aubrites formed by co-crystallization with or exsolution from Ti-poor sulfides (e.g., oldhamite). In the Bustee case, the undetectably low Ti concentrations in oldhamite and experimental Ti partition coefficient between FeS and CaS approaching infinity support such a suggestion. This mechanism solves the long-standing problem of enriching aubritic troilite in Ti and weakens arguments against a direct derivation of aubrites from known enstatite chondrites. | |||||
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 11, p. 32-48, 発行日 1998-03 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |