{"_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"}, "item_12_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "\u4e09\u6ce2\u5ddd\u5909\u6210\u5e2f\u306e\u7070\u66f9\u9577\u77f3-\u9ed2\u96f2\u6bcd\u5e2f\u306b\u304a\u3051\u308b\u6ce5\u8cea\u7247\u5ca9\u306e\u5ca9\u77f3\u5b66\u7684\u7814\u7a76 -\u3068\u304f\u306b\u9ad8\u5727\u4e2d\u9593\u7fa4\u5909\u6210\u4f5c\u7528\u306e\u9ad8\u6e29\u90e8\u306b\u304a\u3051\u308b\u76f8\u5e73\u8861\u306e\u89e3\u6790-"}]}, "item_12_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1983-11-04", "bibliographicIssueDateType": "Issued"}, "bibliographic_titles": [{}]}]}, "item_12_date_granted_64": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u5e74\u6708\u65e5", "attribute_value_mlt": [{"subitem_dategranted": "1983-11-04"}]}, "item_12_description_4": {"attribute_name": "\u6284\u9332", "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 \u00b1 25\u00b0C and 10 \u00b11Kb. 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_type": "Abstract"}]}, "item_12_description_5": {"attribute_name": "\u5185\u5bb9\u8a18\u8ff0", "attribute_value_mlt": [{"subitem_description": "\u540d\u53e4\u5c4b\u5927\u5b66\u535a\u58eb\u5b66\u4f4d\u8ad6\u6587 \u5b66\u4f4d\u306e\u7a2e\u985e:\u7406\u5b66\u535a\u58eb (\u8ab2\u7a0b) \u5b66\u4f4d\u6388\u4e0e\u5e74\u6708\u65e5:\u662d\u548c58\u5e7411\u67084\u65e5", "subitem_description_type": "Other"}]}, "item_12_dissertation_number_65": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u756a\u53f7", "attribute_value_mlt": [{"subitem_dissertationnumber": "13901\u7532\u7b2c1608\u53f7"}]}, "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": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_12_text_14": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}, {"subitem_text_value": "application/pdf"}]}, "item_12_text_63": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u5e74\u5ea6", "attribute_value_mlt": [{"subitem_text_value": "1983"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Enami, Masaki"}], "nameIdentifiers": [{"nameIdentifier": "12109", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u698e\u4e26, \u6b63\u6a39"}], "nameIdentifiers": [{"nameIdentifier": "12110", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "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_free", "mimetype": "application/pdf", "size": 478800.0, "url": {"label": "ko1608_abstr.pdf ", "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_free", "mimetype": "application/pdf", "size": 3100000.0, "url": {"label": "ko1608.pdf ", "url": "https://nagoya.repo.nii.ac.jp/record/4848/files/ko1608.pdf"}, "version_id": "230fec55-1d64-46e6-8ee4-8f9fee17ec2f"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "thesis", "resourceuri": "http://purl.org/coar/resource_type/c_46ec"}]}, "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": "\u30bf\u30a4\u30c8\u30eb", "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"}]}, "item_type_id": "12", "owner": "1", "path": ["336/635/636"], "permalink_uri": "http://hdl.handle.net/2237/6384", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "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": null}