{"created":"2021-03-01T06:11:22.653127+00:00","id":4848,"links":{},"metadata":{"_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":["336:635:636"]},"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","filename":"ko1608_abstr.pdf","filesize":[{"value":"478.8 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","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","filename":"ko1608.pdf","filesize":[{"value":"3.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","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"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2006-05-30"},"publish_date":"2006-05-30","publish_status":"0","recid":"4848","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_creator_id":"1","weko_shared_id":-1},"updated":"2023-01-16T03:49:27.586311+00:00"}