WEKO3
アイテム
{"_buckets": {"deposit": "4b746578-a033-40b0-b302-8465cfbeb349"}, "_deposit": {"created_by": 4, "id": "5966", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "5966"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00005966", "sets": ["777"]}, "author_link": ["43804", "9881", "43803"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2000-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "54", "bibliographicPageStart": "39", "bibliographicVolumeNumber": "13", "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": "Kojima,Tomoko", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "9881", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Yatagai,Tomomi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "43803", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Tomeoka,Kazushige", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "43804", "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 dark inclusion (MNC-1) from the Manych LL (3.1) chondrite contains elliptical objects (\"augen\"; 50-500μm in long axis) embedded in a fine-grained matrix. Most augen are composed of parallel intergrowths of fine laths of Fe-rich olivine, high-Ca pyroxene, and Na-rich feldspathic glass that commonly enclose coarse grains (5-80μm in diameter) of Fe-rich olivine (Fo_\u003c62-83\u003e). The matrix of MNC-1 consists predominantly of interlocking, granular grains (\u003c1-10μm in diameter) of Fe-rich olivine (Fo_\u003c63-66\u003e), interstitial high-Ca pyroxene and Na-rich feldspathic glass. Both the Manych host and MNC-1 have experienced strong shock metamorphism. The texture and mineralogy of MNC-1 suggest that the matrix of MNC-1 experienced shock melting, whereas the \"augen\" represent unmelted precursor material. Bulk major element composition of MNC-1 is generally similar to the average values for LL chondrites, except that MNC-1 is considerably depleted in S and enriched in FeO. The large S depletion may be due to volatilization during impact-induced melting. Texture and mineralogy of the augen are distinct from those of the Manych host, so MNC-1 may not be a melt dike which formed in situ in the host rock. MNC-1 appears to be a xenolith that solidified elsewhere on the LL chondrite parent body and was later incorporated to the present location.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00005966", "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 Earth and Planetary Sciences, Faculty of Science, Kobe University/Department of Earth and Planetary Sciences, Faculty of Science, Kobe University/Department of Earth and Planetary Sciences, Faculty of Science, Kobe University"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2000-03-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000040958.pdf", "filesize": [{"value": "1.8 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1800000.0, "url": {"label": "KJ00000040958", "url": "https://nipr.repo.nii.ac.jp/record/5966/files/KJ00000040958.pdf"}, "version_id": "9f6d25b5-d5b7-4088-8226-2e05d4d08bed"}]}, "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 dark inclusion in the Manych LL (3.1) ordinary chondrite: A product of strong shock metamorphism", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "A dark inclusion in the Manych LL (3.1) ordinary chondrite: A product of strong shock metamorphism"}]}, "item_type_id": "1", "owner": "4", "path": ["777"], "permalink_uri": "https://doi.org/10.15094/00005966", "pubdate": {"attribute_name": "公開日", "attribute_value": "2000-03-01"}, "publish_date": "2000-03-01", "publish_status": "0", "recid": "5966", "relation": {}, "relation_version_is_last": true, "title": ["A dark inclusion in the Manych LL (3.1) ordinary chondrite: A product of strong shock metamorphism"], "weko_shared_id": 4}
A dark inclusion in the Manych LL (3.1) ordinary chondrite: A product of strong shock metamorphism
https://doi.org/10.15094/00005966
https://doi.org/10.15094/000059665835a9bd-ab8b-4144-b53e-95eaca0b2ce2
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000040958 (1.8 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2000-03-01 | |||||
タイトル | ||||||
タイトル | A dark inclusion in the Manych LL (3.1) ordinary chondrite: A product of strong shock metamorphism | |||||
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 | 10.15094/00005966 | |||||
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) |
Kojima,Tomoko
× Kojima,Tomoko× Yatagai,Tomomi× Tomeoka,Kazushige |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Faculty of Science, Kobe University/Department of Earth and Planetary Sciences, Faculty of Science, Kobe University/Department of Earth and Planetary Sciences, Faculty of Science, Kobe University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A dark inclusion (MNC-1) from the Manych LL (3.1) chondrite contains elliptical objects ("augen"; 50-500μm in long axis) embedded in a fine-grained matrix. Most augen are composed of parallel intergrowths of fine laths of Fe-rich olivine, high-Ca pyroxene, and Na-rich feldspathic glass that commonly enclose coarse grains (5-80μm in diameter) of Fe-rich olivine (Fo_<62-83>). The matrix of MNC-1 consists predominantly of interlocking, granular grains (<1-10μm in diameter) of Fe-rich olivine (Fo_<63-66>), interstitial high-Ca pyroxene and Na-rich feldspathic glass. Both the Manych host and MNC-1 have experienced strong shock metamorphism. The texture and mineralogy of MNC-1 suggest that the matrix of MNC-1 experienced shock melting, whereas the "augen" represent unmelted precursor material. Bulk major element composition of MNC-1 is generally similar to the average values for LL chondrites, except that MNC-1 is considerably depleted in S and enriched in FeO. The large S depletion may be due to volatilization during impact-induced melting. Texture and mineralogy of the augen are distinct from those of the Manych host, so MNC-1 may not be a melt dike which formed in situ in the host rock. MNC-1 appears to be a xenolith that solidified elsewhere on the LL chondrite parent body and was later incorporated to the present location. | |||||
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 13, p. 39-54, 発行日 2000-03 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |