WEKO3
アイテム
{"_buckets": {"deposit": "a1797330-78eb-4f4e-97af-5778262d57d5"}, "_deposit": {"created_by": 4, "id": "4678", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "4678"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00004678", "sets": ["592"]}, "author_link": ["8021", "46550", "46549"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1995-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "224", "bibliographicPageStart": "215", "bibliographicVolumeNumber": "8", "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": "Mitreikina,Olga B.", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "8021", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Zinovieva,Nina G.", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "46549", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Granovsky,Lev B.", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "46550", "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": "Detailed studies of ureilites (Novo-Urei, Havero, Dyalpur, Kenna) showed that this type of achondrite had formed in a similar manner to intrusive rocks intensely affected by explosive reducing metal melts rich in hydrocarbon fluids. The reverse zoning of olivine and pyroxene of the ureilite resulted from these alterations. The reverse zoned structure is accompanied by an increase of Mg content in the margins of both minerals and the formation of so-called \"interstitial material\", which is a product of intense recrystallization and partial melting of the olivine and pyroxene at their contacts with metal-carbon veins. The zoning of the primary minerals is controlled by the configuration of the veins. The higher the intensity of the recrystallization process, the more extensive are alterations of the initial rocks exerted by the hydrocarbon fluids, which produced the lherzolite-type pyrope-diamond assemblage.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00004678", "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 Petrology, Faculty of Geology, Moscow State University/Department of Petrology, Faculty of Geology, Moscow State University/Department of Petrology, Faculty of Geology, Moscow State University"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1995-03-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000036484.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": "KJ00000036484", "url": "https://nipr.repo.nii.ac.jp/record/4678/files/KJ00000036484.pdf"}, "version_id": "30fd4502-0b30-4a3a-8b87-f148e064a670"}]}, "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": "Magmatic replacement processes in ureilites", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Magmatic replacement processes in ureilites"}]}, "item_type_id": "1", "owner": "4", "path": ["592"], "permalink_uri": "https://doi.org/10.15094/00004678", "pubdate": {"attribute_name": "公開日", "attribute_value": "1995-03-01"}, "publish_date": "1995-03-01", "publish_status": "0", "recid": "4678", "relation": {}, "relation_version_is_last": true, "title": ["Magmatic replacement processes in ureilites"], "weko_shared_id": 4}
Magmatic replacement processes in ureilites
https://doi.org/10.15094/00004678
https://doi.org/10.15094/000046782e47f457-b131-44bf-bdbb-767605e6f4f7
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000036484 (1.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1995-03-01 | |||||
タイトル | ||||||
タイトル | Magmatic replacement processes in ureilites | |||||
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 | 10.15094/00004678 | |||||
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) |
Mitreikina,Olga B.
× Mitreikina,Olga B.× Zinovieva,Nina G.× Granovsky,Lev B. |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Petrology, Faculty of Geology, Moscow State University/Department of Petrology, Faculty of Geology, Moscow State University/Department of Petrology, Faculty of Geology, Moscow State University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Detailed studies of ureilites (Novo-Urei, Havero, Dyalpur, Kenna) showed that this type of achondrite had formed in a similar manner to intrusive rocks intensely affected by explosive reducing metal melts rich in hydrocarbon fluids. The reverse zoning of olivine and pyroxene of the ureilite resulted from these alterations. The reverse zoned structure is accompanied by an increase of Mg content in the margins of both minerals and the formation of so-called "interstitial material", which is a product of intense recrystallization and partial melting of the olivine and pyroxene at their contacts with metal-carbon veins. The zoning of the primary minerals is controlled by the configuration of the veins. The higher the intensity of the recrystallization process, the more extensive are alterations of the initial rocks exerted by the hydrocarbon fluids, which produced the lherzolite-type pyrope-diamond assemblage. | |||||
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 8, p. 215-224, 発行日 1995-03 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |