{"created":"2023-07-25T11:00:42.548160+00:00","id":2593,"links":{},"metadata":{"_buckets":{"deposit":"ce118b19-5103-4714-9197-a3a1284788fb"},"_deposit":{"created_by":4,"id":"2593","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2593"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002593","sets":["1259:1260:1265:414:417"]},"author_link":["2386","2385","2381"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1989-09","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"127","bibliographicPageStart":"100","bibliographicVolumeNumber":"3","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Antarctic Geosciences"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"GREW, Edward S.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ASAMI, Masao","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"MAKIMOTO, Hiroshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"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":"The eastern Sør Rondane Mountains is largely underlain by biotite and biotite-hornblende quartzo-feldspathic gneisses, in which six rock types occur as lenses ranging from <1m to> 1km in extent : (1) manganese quartzite and iron-rich mafic granulite (2) mafic granulites and amphibolites, (3) ultramafics, (4) garnet-biotite and biotite gneisses, (5) marble and calc-silicate rocks, and (6) cummingtonite ± orthopyroxene orthogneiss. Distinctive mineral assemblages include plagioclase-K-feldspar-fayalite-hedenbergite/augite-ferrosilite-ferropargasitic hornblende-almandine-ilmenite-magnetite-graphite-allanite-pyrrhotite in iron-rich mafic granulite, quartz-spessartine-pyroxmangite-manganoan pigeonite-manganoan augite-manganoan ilmenite (+pyrophanite)-tirodite (secondary) in a manganese quartzite, pyropic garnet-biotite-clinopyroxene-hornblende-anorthite in mafic granulite, sillimanite-garnet-spinel ± corundum (no cordierite) in garnet-biotite gneiss, and forsterite-spinel-calcite and forsterite-diopside-calcite-dolomite in marbles. Secondary minerals include clinohumite, geikielite and Mg-allanite in marble and margarite and hogbomite in amphibolite. Kyanite relics are found in plagioclase in metapelite and with gedrite in garnet in a biotite ± spinel ± corundum schist; these imply pressures above 4kbar on the prograde path. Pressures and temperatures calculated from mineral compositions are &ge;7kbar and 700-750℃ for an early granulite facies event and 500-600℃ for a later, discrete amphibolite facies event. Introduction of rare elements during the latter event and subsequent retrogression in the greenschist facies resulted in the local development of tourmaline, fluorite, allanite (in part) and a mineral of the zirconolite group.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00002593","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":"AA1072335X","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 Geological Sciences, University of Maine"},{"subitem_text_language":"en","subitem_text_value":"Department of Geological Sciences, College of Liberal Arts, Okayama University"},{"subitem_text_language":"en","subitem_text_value":"Geological Survey of Japan"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1989-09-01"}],"displaytype":"detail","filename":"KJ00002368183.pdf","filesize":[{"value":"3.7 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002368183","url":"https://nipr.repo.nii.ac.jp/record/2593/files/KJ00002368183.pdf"},"version_id":"012086d5-19dd-460e-84b6-3d49e4ac2b18"}]},"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":"PRELIMINARY PETROLOGICAL STUDIES OF THE METAMORPHIC ROCKS OF THE EASTERN SØR RONDANE MOUNTAINS","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"PRELIMINARY PETROLOGICAL STUDIES OF THE METAMORPHIC ROCKS OF THE EASTERN SØR RONDANE MOUNTAINS"}]},"item_type_id":"1","owner":"4","path":["417"],"pubdate":{"attribute_name":"公開日","attribute_value":"1989-09-01"},"publish_date":"1989-09-01","publish_status":"0","recid":"2593","relation_version_is_last":true,"title":["PRELIMINARY PETROLOGICAL STUDIES OF THE METAMORPHIC ROCKS OF THE EASTERN SØR RONDANE MOUNTAINS"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:45:04.061905+00:00"}