{"created":"2021-03-01T06:07:47.290418+00:00","id":1426,"links":{},"metadata":{"_buckets":{"deposit":"1b7d1f7b-e411-4e16-b58b-d043ca99d8ab"},"_deposit":{"id":"1426","owners":[],"pid":{"revision_id":0,"type":"depid","value":"1426"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00001426"},"item_9_biblio_info_6":{"attribute_name":"\u66f8\u8a8c\u60c5\u5831","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"102","bibliographicPageStart":"89","bibliographicVolumeNumber":"44","bibliographic_titles":[{"bibliographic_title":"The Journal of earth and planetary sciences, Nagoya University"}]}]},"item_9_description_4":{"attribute_name":"\u6284\u9332","attribute_value_mlt":[{"subitem_description":"The CHIME monazite and xenotime ages were determined for two paragneisses from Madagascar. The biotite-sillimanite-cordierite-quartz-microcline-plagioclase schist at Ihosy in southern Madagascar contains core-mantle monazite grains as well as chronologically unzoned ones. The unzoned monazite grains (8 of 11 analyzed grains) give a CHIME age of 527\u00b115 Ma. Two zoned grains show core ages of 1640\u00b1180 and 797\u00b175 Ma with mantles of 550\u00b150 and 535\u00b110 Ma, respectively. The kyanite- and corundum-bearing cordierite-sillimanite-muscovite-biotite-plagioclase-quartz gneiss at Maevatanana in northwestern Madagascar contains both monazite and xenotime. Monazite and xenotime grains are chronologically uniform, and give CHIME ages of 534\u00b110 and 530\u00b132 Ma, respectively. These chronological data suggest that the high-grade paragneisses in Madagascar, if not all, formed through a single thermal event at ca. 530 Ma from post-797 Ma sediments. This metamorphism can be linked to the continental collision that resulted in Gondwana supercontinent.","subitem_description_type":"Abstract"}]},"item_9_identifier_60":{"attribute_name":"URI","attribute_value_mlt":[{"subitem_identifier_type":"HDL","subitem_identifier_uri":"http://hdl.handle.net/2237/2837"}]},"item_9_identifier_registration":{"attribute_name":"ID\u767b\u9332","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.18999/joueps.44.89","subitem_identifier_reg_type":"JaLC"}]},"item_9_publisher_32":{"attribute_name":"\u51fa\u7248\u8005","attribute_value_mlt":[{"subitem_publisher":"Dept. of Earth and Planetary Sciences, Nagoya University"}]},"item_9_select_15":{"attribute_name":"\u8457\u8005\u7248\u30d5\u30e9\u30b0","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_9_source_id_7":{"attribute_name":"ISSN\uff08print\uff09","attribute_value_mlt":[{"subitem_source_identifier":"0919875X","subitem_source_identifier_type":"ISSN"}]},"item_9_text_14":{"attribute_name":"\u30d5\u30a9\u30fc\u30de\u30c3\u30c8","attribute_value_mlt":[{"subitem_text_value":"application/pdf"}]},"item_creator":{"attribute_name":"\u8457\u8005","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ITO, Masahiro"}],"nameIdentifiers":[{"nameIdentifier":"3322","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"SUZUKI, Kazuhiro"}],"nameIdentifiers":[{"nameIdentifier":"3323","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"YOGO, Setsuo"}],"nameIdentifiers":[{"nameIdentifier":"3324","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":"2018-02-16"}],"displaytype":"detail","filename":"KJ00002415220.pdf","filesize":[{"value":"915.6 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00002415220.pdf","url":"https://nagoya.repo.nii.ac.jp/record/1426/files/KJ00002415220.pdf"},"version_id":"c7b12417-f98b-4aae-ac24-bb03f4c57ef1"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Cambrian granulite to upper amphibolite facies metamorphism of post-797 Ma sediments in Madagascar","item_titles":{"attribute_name":"\u30bf\u30a4\u30c8\u30eb","attribute_value_mlt":[{"subitem_title":"Cambrian granulite to upper amphibolite facies metamorphism of post-797 Ma sediments in Madagascar"}]},"item_type_id":"9","owner":"1","path":["336/337/338/344"],"pubdate":{"attribute_name":"\u516c\u958b\u65e5","attribute_value":"2006-01-05"},"publish_date":"2006-01-05","publish_status":"0","recid":"1426","relation_version_is_last":true,"title":["Cambrian granulite to upper amphibolite facies metamorphism of post-797 Ma sediments in Madagascar"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2021-03-01T21:37:13.905607+00:00"}