{"created":"2021-03-01T06:30:08.059352+00:00","id":22376,"links":{},"metadata":{"_buckets":{"deposit":"c4b2d622-c06a-41db-b30c-51c309d46bae"},"_deposit":{"id":"22376","owners":[],"pid":{"revision_id":0,"type":"depid","value":"22376"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00022376"},"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 metamorphic rocks of the Gyeonggi massif in the Korean Peninsula"}]},"item_9_biblio_info_6":{"attribute_name":"\u66f8\u8a8c\u60c5\u5831","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"100","bibliographicPageStart":"95","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":"Metamorphic rocks in the northeastern part of the Gyeonggi massif in the Korean Peninsula include pelitic and quartzofeldspathic granulites, augen gneiss, paragneiss in the amphibolite-facies and amphibolite, and are grouped into the high-grade granulite- and the low-grade gneiss-units. The tectonically lower granulite unit is separated from the gneiss unit by an extensive mylonite zone that show a metamorphic overprint characterized by the fibrolite and K-feldspar paragenesis. Pelitic and quartzofeldspathic granulites in the granulite unit give Paleoproterozoic (1.84-1.89 Ga) CHIME monazite ages, whereas paragneisses in the gneiss unit and rocks in the mylonite zone yield unequivocal Early Triassic (240\u00b110 Ma) ages. Augen gneiss and mylonitized pelitic granulite underlain below the mylonite zone yield Early Triassic age domains on and within predominantly Paleoproterozoic monazite grains. Augen gneiss as well as mylonite shows a consistent top-to-the-NE shear sense with gently inclined NE-SW mineral alignments. The chronological and structural data suggest that the juxtaposition of the hot gneiss unit by thrusting over the granulite unit was responsible for the Early Triassic overprint in the granulite unit and in the mylonite zone. The gneiss unit was possibly detached from the South China block during the collision between the North China and South China blocks, and was distributed as widespread allochthons on the granulite unit of the North China block. \u30b3\u30ea\u30a2\u534a\u5cf6\u4e2d\u90e8\uff0c\u4eac\u757f\u5730\u584a\u306e\u5909\u6210\u5ca9\u306f\u53e4\u539f\u751f\u4ee3(\u7d0418.4-18.9\u5104\u5e74)\u306e\u30b0\u30e9\u30cb\u30e5\u30e9\u30a4\u30c8\u30e6\u30cb\u30c3\u30c8\u3068\u4e09\u7573\u7d00\u521d\u982d(240\u00b110 Ma)\u306e\u7247\u9ebb\u5ca9\u30e6\u30cb\u30c3\u30c8\u304b\u3089\u69cb\u6210\u3055\u308c\u308b\uff0e\u5883\u754c\u306b\u306f\u5927\u898f\u6a21\u306a\u30de\u30a4\u30ed\u30ca\u30a4\u30c8\u5e2f\u304c\u767a\u9054\u3057\uff0c\u30de\u30a4\u30ed\u30ca\u30a4\u30c8\u81ea\u4f53\u304c\u4e09\u7573\u7d00\u521d\u982d(240\u00b110 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