{"_buckets": {"deposit": "8908f98b-cd53-4e68-9933-dc429ef1d6aa"}, "_deposit": {"id": "4848", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "4848"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00004848", "sets": ["636"]}, "author_link": ["12109", "12110"], "item_12_alternative_title_19": {"attribute_name": "その他のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "三波川変成帯の灰曹長石-黒雲母帯における泥質片岩の岩石学的研究 -とくに高圧中間群変成作用の高温部における相平衡の解析-", "subitem_alternative_title_language": "ja"}]}, "item_12_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1983-11-04", "bibliographicIssueDateType": "Issued"}}]}, "item_12_date_granted_64": {"attribute_name": "学位授与年月日", "attribute_value_mlt": [{"subitem_dategranted": "1983-11-04"}]}, "item_12_degree_grantor_62": {"attribute_name": "学位授与機関", "attribute_value_mlt": [{"subitem_degreegrantor": [{"subitem_degreegrantor_language": "ja", "subitem_degreegrantor_name": "名古屋大学"}, {"subitem_degreegrantor_language": "en", "subitem_degreegrantor_name": "Nagoya University"}], "subitem_degreegrantor_identifier": [{"subitem_degreegrantor_identifier_name": "13901", "subitem_degreegrantor_identifier_scheme": "kakenhi"}]}]}, "item_12_degree_name_61": {"attribute_name": "学位名", "attribute_value_mlt": [{"subitem_degreename": "理学博士", "subitem_degreename_language": "ja"}]}, "item_12_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The oligoclase-biotite zone of the Bessi area, central Shikoku is characterized by sodic plagioclase-bearing assemblages in pelitickl schists, and resents the highest-grade zone of the Sanbagawa metamorphic terrain. Mineral assemblages of pelitic schists in this zone, all with quartz, sodic plagioclase, muscovite and clinozoisite (or zoisite), are garnet + biotite + chlorite + paragonite, garnet + biotite + hornblende +chlorite, and partial assemblages of the above types. Correlations between mineral compositions, mineral assemblages and mineral stability date assuming suggest that metamorphic conditions of this zone are about 610 ± 25°C and 10 ±1Kb. Based upon the comparative study of mineralogy and chemistry of pelitic schists in the oligoclase-biotite zone with those in New Caledonia omphacite zone as a typical high-pressure type and with those in upper staurolite zone as medium-pressure type, progressive as semblages within these zones can be related by such reactions as: omphacite zone garnet + glaucophane + omphacite + muscovite = oligoclase-biotite zone biotite + hornblende + plagioclase + quartz + H2O oligoclase-biotite zone garnet + hornblende + paragonite + muscovite = upper staurolite zone staurolite + biotite + plagioclase + quartz +H2O dP/dT values of these equations calculated using natural compositions are 3-6 and 16-19, respectivel, and their gradients are gentle. This implies that the contrasts of mineral parageneses in pelitic schists related by the aboveequations result mainly from the difference in pressure during progressive metamorphism. A combination of mineral assemblages observed in the Sanbagawa oligoclase-biotite zone represents a characteristic mineral paragenesis of pelitic schists in the high-grade part of an intermediate high-pressure metamorphism.", "subitem_description_language": "en", "subitem_description_type": "Abstract"}]}, "item_12_description_5": {"attribute_name": "内容記述", "attribute_value_mlt": [{"subitem_description": "名古屋大学博士学位論文 学位の種類:理学博士 (課程) 学位授与年月日:昭和58年11月4日", "subitem_description_language": "ja", "subitem_description_type": "Other"}]}, "item_12_dissertation_number_65": {"attribute_name": "学位授与番号", "attribute_value_mlt": [{"subitem_dissertationnumber": "甲第1608号"}]}, "item_12_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/6384"}]}, "item_12_select_15": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_12_text_14": {"attribute_name": "フォーマット", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}, {"subitem_text_value": "application/pdf"}]}, "item_12_text_63": {"attribute_name": "学位授与年度", "attribute_value_mlt": [{"subitem_text_value": "1983"}]}, "item_access_right": {"attribute_name": "アクセス権", "attribute_value_mlt": [{"subitem_access_right": "open access", "subitem_access_right_uri": "http://purl.org/coar/access_right/c_abf2"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Enami, Masaki", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "12109", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "榎並, 正樹", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "12110", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-19"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "ko1608_abstr.pdf", "filesize": [{"value": "478.8 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 478800.0, "url": {"label": "ko1608_abstr.pdf ", "objectType": "abstract", "url": "https://nagoya.repo.nii.ac.jp/record/4848/files/ko1608_abstr.pdf"}, "version_id": "5df71798-8d44-4aae-a60b-1afbc4cc40f6"}, {"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-19"}], "displaytype": "detail", "download_preview_message": "", "file_order": 1, "filename": "ko1608.pdf", "filesize": [{"value": "3.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 3100000.0, "url": {"label": "ko1608.pdf ", "objectType": "fulltext", "url": "https://nagoya.repo.nii.ac.jp/record/4848/files/ko1608.pdf"}, "version_id": "230fec55-1d64-46e6-8ee4-8f9fee17ec2f"}]}, "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": "doctoral thesis", "resourceuri": "http://purl.org/coar/resource_type/c_db06"}]}, "item_title": "Petrology of Pelitic Schists in the Oligoclase-Biotite Zone of the Sanbagawa Metamorphic Terrain,Japan: Phase Equilibria in High-Grade Zone of an Intermediate High-Pressure Metamorphism", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Petrology of Pelitic Schists in the Oligoclase-Biotite Zone of the Sanbagawa Metamorphic Terrain,Japan: Phase Equilibria in High-Grade Zone of an Intermediate High-Pressure Metamorphism", "subitem_title_language": "en"}]}, "item_type_id": "12", "owner": "1", "path": ["636"], "permalink_uri": "http://hdl.handle.net/2237/6384", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2006-05-30"}, "publish_date": "2006-05-30", "publish_status": "0", "recid": "4848", "relation": {}, "relation_version_is_last": true, "title": ["Petrology of Pelitic Schists in the Oligoclase-Biotite Zone of the Sanbagawa Metamorphic Terrain,Japan: Phase Equilibria in High-Grade Zone of an Intermediate High-Pressure Metamorphism"], "weko_shared_id": -1}