{"_buckets": {"deposit": "db8c3698-3281-4b82-a46d-cc58c2f4688c"}, "_deposit": {"id": "22367", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "22367"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00022367"}, "item_9_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "CHIME monazite ages of the Hikami Granite and the Ono Formation in the South Kitakami Terrane"}]}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2016-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "51", "bibliographicPageStart": "46", "bibliographicVolumeNumber": "27", "bibliographic_titles": [{"bibliographic_title": "\u540d\u53e4\u5c4b\u5927\u5b66\u52a0\u901f\u5668\u8cea\u91cf\u5206\u6790\u8a08\u696d\u7e3e\u5831\u544a\u66f8"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The geologic relation between the Hikami Granite and the fossiliferous Siluro-Devonian strata in the South Kitakami terrane has long been an open problem. Detailed CHIME dating and elemental mapping of monazite from the southern part (Hinokamiyama type) of the granite disclose ubiquitous development of Late Devonian (365\u00b134 Ma) mantles on Silurian cores. Monazite-free granite samples (Ono type) from the northern part give a 373\u00b135 Ma Rb-Sr whole-rock isochron age with R1=0.70669\u00b10.00037, suggesting to be a possible heat source for the Late Devonian overprint on the Hinokamiyama type. The CHIME monazite dating also revealed (1) the granite at Kusayami-zawa, believed as the part of the Hikami Granite and interpreted to be covered unconformably by the Silurian arkose, is of Cretaceous (123\u00b16 Ma), (2) the Silurian arkose contains Ordovician monazite without Post-Silurian age signature, (3) an arkose bed intercalated in the Devonian Ono Formation contains unequivocal Cretaceous (113\u00b112 Ma) monazite grains, and (4) a porphyroblastic facies, being ascribed sometimes as mylonite, within the Hikami Granite contains Silurian-Late Devonian and Silurian-Late Devonian-Permian zoned monazite grains together with chronologically uniform Silurian and Cretaceous monazite grains. The porphyroblastic facies is likely to be a granitic arkose. These lines of geochronological evidence suggest that the Hikami Granite and the fossiliferous Silurian and Devonian strata are exotic blocks enclosed within a Cretaceous m\u00e9lange. 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