{"created":"2023-07-25T10:59:48.573954+00:00","id":1559,"links":{},"metadata":{"_buckets":{"deposit":"dcfc0767-14e3-4ff8-9266-0c08ad7f242c"},"_deposit":{"created_by":4,"id":"1559","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"1559"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00001559","sets":["1:356:384"]},"author_link":["65174","58580","57969","56255","65366","58582"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1983-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"205","bibliographicPageStart":"181","bibliographicVolumeNumber":"30","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Takeda, Hiroshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Mori, Hiroshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Delaney, J.S.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Prinz, M.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Harlow, G.E.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Ishii, Teruaki","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":"Mineralogical examination of thin sections of non-Antarctic and Antarctic HED (howardite, eucrite, diogenite) achondrites indicates that they contain a variety of lithic components. Some of these components occur both as monomict meteorites and as clasts in polymict meteorites, whereas others occur only as clasts in some polymict breccias. The components may be classified by the degree of homogenization of the pyroxene present. In order of increasing homogeneity these are : (1) Y-75011-type basalt clasts; (2) Pasamonte; (3) Y-790266-type clasts; (4) Stannern and Nuevo Laredo; (5) Juvinas and Haraiya; and (6) Ibitira (?). Type 1 has been least modified by post-igneous thermal annealing, while types 5 and 6 were thoroughly metamorphosed. Three types of cumulate eucrites are recognized and are believed to represent (a) cumulates from thick lava flows or layered intrusions; (b) lunar highlands type crust; and (c) differentiation products of diogenitic magmas.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","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":"Mineralogical Institute, Faculty of Science, University of Tokyo/Mineralogical Institute, Faculty of Science, University of Tokyo/Department of Mineral Sciences, Americal Museum of Natural History/Department of Mineral Sciences, Americal Museum of Natural History/Department of Mineral Sciences, Americal Museum of Natural History/Ocean Research Institute,University of Tokyo"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1983-12-01"}],"displaytype":"detail","filename":"KJ00000012192.pdf","filesize":[{"value":"3.3 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"url":"https://nipr.repo.nii.ac.jp/record/1559/files/KJ00000012192.pdf"},"version_id":"6147538b-a34f-43d5-82fd-3ed1794c70c8"}]},"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":"Mineralogical comparison of Antarctic and non-Antarctic HED (howardites-eucrites-diogenites) achondrites","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Mineralogical comparison of Antarctic and non-Antarctic HED (howardites-eucrites-diogenites) achondrites","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["384"],"pubdate":{"attribute_name":"公開日","attribute_value":"1983-12-01"},"publish_date":"1983-12-01","publish_status":"0","recid":"1559","relation_version_is_last":true,"title":["Mineralogical comparison of Antarctic and non-Antarctic HED (howardites-eucrites-diogenites) achondrites"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:47:31.035342+00:00"}