Integrated Zircon U-Pb-O-Hf and Whole-Rock Sm-Nd Studies of Paleozoic Amphibolites in the Chencai Area of the Cathaysia Block, South China

doi:10.1086/699927

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	Integrated Zircon U-Pb-O-Hf and Whole-Rock Sm-Nd Studies of Paleozoic Amphibolites in the Chencai Area of the Cathaysia Block, South China
	Zhao, Lei 1,2; Liu, Bo 1,3; Nutman, Allen P.2; Zhai, Mingguo 1,4; Zhou, Xiwen 5; Cui, Xiahong 1,3
刊名	JOURNAL OF GEOLOGY
	2018-11-01
卷号	126 期号:6 页码:621-637
ISSN号	0022-1376
DOI	10.1086/699927
英文摘要	The present metamorphic crystalline basement of the South China Block was formed largely as a result of the early Paleozoic (similar to 460-410 Ma) orogeny, which affected large areas of this continental block. Paleozoic metamafic rocks (garnet amphibolites) with typical normal mid-ocean ridge basalt chemical compositions were recently identified from an uplifted lower-crustal rock assemblage in the Chencai area of the Cathaysia Block. This article focuses on the first integrated studies of secondary-ion mass spectroscopy (SIMS) zircon U-Pb dating and zircon Lu-Hf-O and whole-rock Sm-Nd isotopic analyses on these metamafic rocks, for the purpose of better constraining the ancient geodynamic processes of this orogeny. The SIMS zircon U-Pb dating results show that these mafic rocks underwent high-grade metamorphismat similar to 427 Ma, within the time span of Paleozoic orogeny. Most zircon Lu-Hf and O isotopic results display relatively uniform compositions, with delta O-18 values scattering around +9 parts per thousand and the calculated epsilon(Hf)(t) values of most metamorphic zircons ranging from +9.8 to +15.1. The Nd-143/Nd-144 and Sm-147/Nd-144 ratios of the three samples are 0.513075-0.513103 and 0.20508-0.205832, respectively. The epsilon(Nd)(t) values are high positive, ranging from +8.05 to +8.63. These ratios resemble those of basaltic rocks newly derived from a depleted-mantle source. Zircon Hf model ages are similar to 540 Ma, older than the previous result of similar to 496 Ma, suggesting that these newly formed crustal materials were likely extracted from the depleted-mantle source during the early Paleozoic. It is thus inferred from such isotopic characteristics, as well as previously published data of the metamafic rocks, that the previous notion-that a deep lithospheric fracture reaching asthenospheric mantle was absent from the Early Paleozoic South China Orogen-should be reconsidered.
资助项目	National Nature Science Foundation of China[41502182] ; National Nature Science Foundation of China[41530208] ; National Nature Science Foundation of China[41210003] ; National Nature Science Foundation of China[41372196] ; China Geological Survey[1212010811048] ; China Geological Survey[12120114064301] ; China Postdoctoral Science Foundation[2016T90133] ; China Scholarship Council[201604910053]
WOS关键词	NEOPROTEROZOIC TECTONIC EVOLUTION ; IONIZATION MASS-SPECTROMETRY ; JIANGNAN OROGEN ; LU-HF ; VOLCANIC-ROCKS ; CONTINENTAL COLLISION ; SOUTHEASTERN CHINA ; KWANGSIAN OROGENY ; MAFIC INTRUSIONS ; FACIES ZIRCONS
WOS研究方向	Geology
语种	英语
出版者	UNIV CHICAGO PRESS
WOS记录号	WOS:000449866400004
资助机构	National Nature Science Foundation of China ; National Nature Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Scholarship Council ; China Scholarship Council ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Scholarship Council ; China Scholarship Council ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Scholarship Council ; China Scholarship Council ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Scholarship Council ; China Scholarship Council
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/89427]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者	Zhao, Lei
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Univ Wollongong, Sch Earth & Environm Sci, GeoQuEST Res Ctr, Wollongong, NSW 2522, Australia 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Univ Chinese Acad Sci, Key Lab Computat Geodynam, Beijing 100049, Peoples R China 5.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
推荐引用方式 GB/T 7714	Zhao, Lei,Liu, Bo,Nutman, Allen P.,et al. Integrated Zircon U-Pb-O-Hf and Whole-Rock Sm-Nd Studies of Paleozoic Amphibolites in the Chencai Area of the Cathaysia Block, South China[J]. JOURNAL OF GEOLOGY,2018,126(6):621-637.
APA	Zhao, Lei,Liu, Bo,Nutman, Allen P.,Zhai, Mingguo,Zhou, Xiwen,&Cui, Xiahong.(2018).Integrated Zircon U-Pb-O-Hf and Whole-Rock Sm-Nd Studies of Paleozoic Amphibolites in the Chencai Area of the Cathaysia Block, South China.JOURNAL OF GEOLOGY,126(6),621-637.
MLA	Zhao, Lei,et al."Integrated Zircon U-Pb-O-Hf and Whole-Rock Sm-Nd Studies of Paleozoic Amphibolites in the Chencai Area of the Cathaysia Block, South China".JOURNAL OF GEOLOGY 126.6(2018):621-637.