{"created":"2023-06-20T14:52:29.174205+00:00","id":20635,"links":{},"metadata":{"_buckets":{"deposit":"03822471-4539-4b38-aedd-91e24a724111"},"_deposit":{"created_by":1,"id":"20635","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"20635"},"status":"published"},"_oai":{"id":"oai:jaxa.repo.nii.ac.jp:00020635","sets":["1543:1778:1792","1887:1891"]},"author_link":["196793","196798","196797","196795","196799","196796","196800","196794"],"item_5_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"拡散の修正によって計算したパラサイトに対する冷却速度の評価:カンラン石のFe-MgおよびCaOのゾーニング"}]},"item_5_biblio_info_10":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2004-02","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"227","bibliographicPageStart":"224","bibliographic_titles":[{"bibliographic_title":"第37回月・惑星シンポジウム"},{"bibliographic_title":"Proceedings of the 37th ISAS Lunar and Planetary Symposium","bibliographic_titleLang":"en"}]}]},"item_5_description_17":{"attribute_name":"抄録（英）","attribute_value_mlt":[{"subitem_description":"The cooling rate (and burial depth) was recalculated by using different diffusion coefficients from those used in the previous studies on the basis of the Fe-Mg and CaO chemical zoning profiles observed for pallasite (Esquel) olivine. The cooling rate obtained from the Fe-Mg zoning profile is broadly consistent with that from the CaO profile and is 2 to 5 C/yr (300 to 200 m in depth) for cooling from 1,100 C. The results of recalculation for the cooling rate also show a relatively fast cooling at the high-temperature range. Therefore, a shallow origin for pallasites during high temperature should be further explored.","subitem_description_type":"Other"}]},"item_5_description_32":{"attribute_name":"資料番号","attribute_value_mlt":[{"subitem_description":"資料番号: AA0047898057","subitem_description_type":"Other"}]},"item_5_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"宇宙航空研究開発機構宇宙科学研究本部"}]},"item_5_publisher_9":{"attribute_name":"出版者（英）","attribute_value_mlt":[{"subitem_publisher":"Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA/ISAS)"}]},"item_5_text_6":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"東京大学 大学院理学系研究科"},{"subitem_text_value":"東京大学 大学院理学系研究科"},{"subitem_text_value":"東京大学 大学院理学系研究科"},{"subitem_text_value":"東京大学 大学院理学系研究科"}]},"item_5_text_7":{"attribute_name":"著者所属（英）","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"University of Tokyo Graduate School of Science"},{"subitem_text_language":"en","subitem_text_value":"University of Tokyo Graduate School of Science"},{"subitem_text_language":"en","subitem_text_value":"University of Tokyo Graduate School of Science"},{"subitem_text_language":"en","subitem_text_value":"University of Tokyo Graduate School of Science"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"宮本, 正道"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"小泉, 英祐"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"三河内, 岳"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"鳥海, 淳"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Miyamoto, Masamichi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Koizumi, Eisuke","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Mikochi, Takashi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Chokai, Jun","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Fe-Mg帯状分布","subitem_subject_scheme":"Other"},{"subitem_subject":"CaO帯状分布","subitem_subject_scheme":"Other"},{"subitem_subject":"拡散変態","subitem_subject_scheme":"Other"},{"subitem_subject":"拡散係数","subitem_subject_scheme":"Other"},{"subitem_subject":"カンラン石","subitem_subject_scheme":"Other"},{"subitem_subject":"冷却速度","subitem_subject_scheme":"Other"},{"subitem_subject":"計算","subitem_subject_scheme":"Other"},{"subitem_subject":"高温","subitem_subject_scheme":"Other"},{"subitem_subject":"Fe-Mg zoning","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"CaO zoning","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"diffusional modification","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"diffusion coefficient","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"olivine","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"cooling rate","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"computation","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"high temperature","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"conference paper","resourceuri":"http://purl.org/coar/resource_type/c_5794"}]},"item_title":"Evaluation of the cooling rate for pallasite calculated by diffusional modification: Fe-Mg and CaO zoning of olivine","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Evaluation of the cooling rate for pallasite calculated by diffusional modification: Fe-Mg and CaO zoning of olivine","subitem_title_language":"en"}]},"item_type_id":"5","owner":"1","path":["1792","1891"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-03-26"},"publish_date":"2015-03-26","publish_status":"0","recid":"20635","relation_version_is_last":true,"title":["Evaluation of the cooling rate for pallasite calculated by diffusional modification: Fe-Mg and CaO zoning of olivine"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-21T03:47:26.664597+00:00"}