The Early Permian active continental margin and crustal growth of the Cathaysia Block: In situ U-Pb, Lu-Hf and O isotope analyses of detrital zircons

doi:10.1016/j.chemgeo.2011.10.027

	The Early Permian active continental margin and crustal growth of the Cathaysia Block: In situ U-Pb, Lu-Hf and O isotope analyses of detrital zircons
	Li, Xian-Hua 1,2; Li, Zheng-Xiang 3; He, Bin 2; Li, Wu-Xian 2; Li, Qiu-Li 1; Gao, Yuya 1; Wang, Xuan-Ce 1,3
刊名	CHEMICAL GEOLOGY
	2012-10-18
卷号	328 页码:195-207
关键词	Detrital zircon U-Pb age Hf and O isotopes Permian Sedimentary provenance Southeastern China
ISSN号	0009-2541
DOI	10.1016/j.chemgeo.2011.10.027
文献子类	Article
英文摘要	Late Permian to Triassic ("Indosinian-aged") orogenesis and associated magmatism are widespread in southeastern China, but their causes and significance to the regional geodynamic evolution are highly controversial. We report in this study integrated in situ U-Pb, Hf and O isotope analyses of detrital zircons from the Middle to Late Permian sediments in southeastern China, and use these data to decipher the sedimentary provenances, regional magmatic barcode and crustal evolution processes. A total of 409 concordant U-Pb zircon analyses on five sedimentary samples exhibits four major age peaks at ca 1870 Ma, ca 445 Ma, ca 370 Ma and ca 280 Ma, one "broad" age group of ca 1180-960 Ma, and two subordinate peaks at ca 2530 Ma and ca 800 Ma All the Archean-aged detrital zircons are oval in shape with clear abrasive imprints, indicating long-distance transport and/or multi-cycled sedimentary processing from unknown Archean sources. In contrast, detrital zircons of the remaining age groups are mostly euhedral to subhedral crystals, suggesting short-distance transport. Zircon ages of ca 1870 Ma, ca 1180-960 Ma, ca 800 Ma, ca 445 Ma and ca 280 Ma are coeval with exposed magmatic rocks in the Cathaysia Block of southeastern China. The ubiquitous existence of ca 280 Ma detrital zircons in the studied sediments implies a widespread occurrence of Early Permian magmatic rocks in southeastern China coastal region.
WOS关键词	SOUTH CHINA CONSTRAINTS ; INDOSINIAN OROGENY ; YANGTZE CRATON ; VOLCANIC-ROCKS ; TRACE-ELEMENT ; HAINAN ISLAND ; TECTONIC EVOLUTION ; VELOCITY STRUCTURE ; 2-STAGE MODEL ; MAGMATIC ARC
WOS研究方向	Geochemistry & Geophysics
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000310124900012
资助机构	Chinese Academy of Sciences(XDA08110400) ; Chinese Academy of Sciences(XDA08110400) ; Ministry of Science and Technology(2012CB416702 ; Ministry of Science and Technology(2012CB416702 ; National Natural Science Foundation of China(40728002) ; National Natural Science Foundation of China(40728002) ; Australian Research Council(DP110104799) ; Australian Research Council(DP110104799) ; 2007CB411403) ; 2007CB411403) ; Chinese Academy of Sciences(XDA08110400) ; Chinese Academy of Sciences(XDA08110400) ; Ministry of Science and Technology(2012CB416702 ; Ministry of Science and Technology(2012CB416702 ; National Natural Science Foundation of China(40728002) ; National Natural Science Foundation of China(40728002) ; Australian Research Council(DP110104799) ; Australian Research Council(DP110104799) ; 2007CB411403) ; 2007CB411403) ; Chinese Academy of Sciences(XDA08110400) ; Chinese Academy of Sciences(XDA08110400) ; Ministry of Science and Technology(2012CB416702 ; Ministry of Science and Technology(2012CB416702 ; National Natural Science Foundation of China(40728002) ; National Natural Science Foundation of China(40728002) ; Australian Research Council(DP110104799) ; Australian Research Council(DP110104799) ; 2007CB411403) ; 2007CB411403) ; Chinese Academy of Sciences(XDA08110400) ; Chinese Academy of Sciences(XDA08110400) ; Ministry of Science and Technology(2012CB416702 ; Ministry of Science and Technology(2012CB416702 ; National Natural Science Foundation of China(40728002) ; National Natural Science Foundation of China(40728002) ; Australian Research Council(DP110104799) ; Australian Research Council(DP110104799) ; 2007CB411403) ; 2007CB411403)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/84226]
专题	中国科学院地质与地球物理研究所
通讯作者	Li, Xian-Hua
作者单位	1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China 3.Curtin Univ Technol, Dept Appl Geol, Inst Geosci Res TIGeR, Perth, WA 6845, Australia
推荐引用方式 GB/T 7714	Li, Xian-Hua,Li, Zheng-Xiang,He, Bin,et al. The Early Permian active continental margin and crustal growth of the Cathaysia Block: In situ U-Pb, Lu-Hf and O isotope analyses of detrital zircons[J]. CHEMICAL GEOLOGY,2012,328:195-207.
APA	Li, Xian-Hua.,Li, Zheng-Xiang.,He, Bin.,Li, Wu-Xian.,Li, Qiu-Li.,...&Wang, Xuan-Ce.(2012).The Early Permian active continental margin and crustal growth of the Cathaysia Block: In situ U-Pb, Lu-Hf and O isotope analyses of detrital zircons.CHEMICAL GEOLOGY,328,195-207.
MLA	Li, Xian-Hua,et al."The Early Permian active continental margin and crustal growth of the Cathaysia Block: In situ U-Pb, Lu-Hf and O isotope analyses of detrital zircons".CHEMICAL GEOLOGY 328(2012):195-207.