New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan:;Implications for tectonic correlation with Jiamushi massif

doi:10.1111/iar.12045

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	New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan:;Implications for tectonic correlation with Jiamushi massif
	Zhao, Xilin 3; Mao, Jianren ; Ye, Haimin ; Liu, Kai ; Takahashi, Yutaka 1
刊名	ISLAND ARC
	2013
卷号	22 期号:4 页码:508-521
关键词	Central Asian Orogenic Belt Hida Belt Jiamushi massif SHRIMP U-Pb zircon dating
ISSN号	1038-4871;EI 1440-1738
DOI	10.1111/iar.12045
英文摘要	Granitoids in the Hida region of Japan encompass two main rock types: younger type-1 granites and older type-2 granites. Sensitive high mass-resolution ion microprobe (SHRIMP) U-Pb zircon dating of older type-2 granites collected from the Tateyama area show similar ages of 245 +/- 2Ma and 248 +/- 5Ma for two gneissose granites, while a significantly younger intrusion age of 197 +/- 3Ma was determined for the younger type-1 granites collected from the Hayatsukigawa River which belongs to the Okumayama pluton. A felsic gneiss sample (07HI-3) collected from the right bank of the Hayatsukigawa River yielded multiple complex ages at 330 +/- 6Ma, indicating the timing of the Hida regional tectono-thermal events that formed the Hida gneisses; 243 +/- 8Ma, representing the timing of intrusion of the augen granite; and 220Ma, indicating the timing of regional dextral ductile shearing that caused a repeated recrystallization of metamorphic rocks in the study area. Considering the geochronological data, the rock types and assemblages, basement, and Sr-Nd isotopic constraints, we propose that the Hida Belt separated from the Jiamushi massif, which is located in the eastern margin of the Central Asian Orogenic Belt.
学科主题	火成岩岩石学
WOS关键词	SOUTH-KOREA ; METAMORPHIC BELTS ; CHEMICAL CHARACTERISTICS ; NORTHEASTERN ; CHINA ; CONSTRAINTS ; EVOLUTION ; ISLANDS ; EAST ; ASIA ; GEOCHRONOLOGY
WOS研究方向	Geology
语种	英语
出版者	WILEY-BLACKWELL
WOS记录号	WOS:000330122200005
内容类型	期刊论文
源URL	[http://119.78.100.197/handle/2HKVOGP0/39953]
专题	中国地质调查局南京地质调查中心
作者单位	1.Nangjing Inst Geol & Mineral Resources, Nanjing 210016, Jiangsu, Peoples R China. 2.Geol Survey Japan, Inst Geol & Geoinformat Ctr, AIST, Tsukuba, Ibaraki 3058567, Japan. 3.中国地质调查局南京地质调查中心
推荐引用方式 GB/T 7714	Zhao, Xilin,Mao, Jianren,Ye, Haimin,et al. New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan:;Implications for tectonic correlation with Jiamushi massif[J]. ISLAND ARC,2013,22(4):508-521.
APA	Zhao, Xilin,Mao, Jianren,Ye, Haimin,Liu, Kai,&Takahashi, Yutaka.(2013).New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan:;Implications for tectonic correlation with Jiamushi massif.ISLAND ARC,22(4),508-521.
MLA	Zhao, Xilin,et al."New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan:;Implications for tectonic correlation with Jiamushi massif".ISLAND ARC 22.4(2013):508-521.