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Detrital Zircons U-Pb Age and Hf Isotope from the Western Side of the Taiwan Strait: Implications for Sediment Provenance and Crustal Evolution of the Northeast Cathaysia Block

文献类型：期刊论文

作者Xu, Yonghang1; Sun, Qinqin2; Yi, Liang3; Yin, Xijie1; Wang, Aijun1; Li, Yunhai1; Chen, Jian1
刊名TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES
出版日期2014-08-01
卷号25期号:4页码:505-535
ISSN号1017-0839
关键词Detrital zircon U-Pb age Hf isotope Provenance Crustal evolution Cathaysia Block
DOI10.3319/TAO.2014.02.18.01(TT)
文献子类Article
英文摘要In situ detrital zircons U-Pb and Hf isotope analyses from the Min and Jiulong River of Southeast China were carried out to identify sediment provenance and crustal evolution of the northeast Cathaysia Block. Detrital zircons from both rivers displayed similar spectrum peaks at 236, 155, and 110 Ma, but samples from the Min River displayed a distinct Caledonian peak (ca. 460 Ma) and contained more Precambrian particles (ca. 1.8 Ga), which likely stemmed from the upstream area of the Wuyishan terrain. Interestingly, because Taiwan Island cannot supply Caledonian and Paleoproterozoic detrital materials and because the Ou and Jiulong River also lack components from these two populations, it is highly likely that the sediment in the western Taiwan coast partially originates from the Min River. The sediments from the Min River in Fujian are also considered the most likely source of the beach sands of western Taiwan (Chen et al. 2006). However, we stress that the 1.8 Ga age source in the western Taiwan sediments was found and recognized. Combining U-Pb dating and Hf-isotope suggests that the northeast Cathaysia Block contains some Neoarchean detrital zircons, which derived from the incorporation of juvenile mantle materials and re-melting of ancient crustal substances. The wide ranges of epsilon(HF)(t) value in the Paleoproterozoic and Neoproterozoic demonstrate the re-melting of ancient crustal materials with minor juvenile mantle materials. Phanerozoic zircons stemmed from re-melting and recycling of Proterozoic crustal materials with or without the invasion of juvenile mantle-derived magmas.
WOS关键词SOUTH CHINA ; LU-HF ; SE CHINA ; CONTINENTAL-CRUST ; RIVER SYSTEM ; GEOCHRONOLOGY ; CONSTRAINTS ; OROGEN ; GEOCHEMISTRY ; REWORKING
WOS研究方向Geology ; Meteorology & Atmospheric Sciences ; Oceanography
语种英语
出版者CHINESE GEOSCIENCE UNION
WOS记录号WOS:000340218000004
资助机构National Natural Science Foundation of China(NSFC 40906047 ; National Natural Science Foundation of China(NSFC 40906047 ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Natural Science Foundation of Fujian Province(2010J05096) ; Natural Science Foundation of Fujian Province(2010J05096) ; 41106073) ; 41106073) ; National Natural Science Foundation of China(NSFC 40906047 ; National Natural Science Foundation of China(NSFC 40906047 ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Natural Science Foundation of Fujian Province(2010J05096) ; Natural Science Foundation of Fujian Province(2010J05096) ; 41106073) ; 41106073) ; National Natural Science Foundation of China(NSFC 40906047 ; National Natural Science Foundation of China(NSFC 40906047 ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Natural Science Foundation of Fujian Province(2010J05096) ; Natural Science Foundation of Fujian Province(2010J05096) ; 41106073) ; 41106073) ; National Natural Science Foundation of China(NSFC 40906047 ; National Natural Science Foundation of China(NSFC 40906047 ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Scientific Research Foundation of Third Institute of Oceanography (SOA.)(2014015) ; Natural Science Foundation of Fujian Province(2010J05096) ; Natural Science Foundation of Fujian Province(2010J05096) ; 41106073) ; 41106073)
源URL[http://ir.iggcas.ac.cn/handle/132A11/85468]  
专题中国科学院地质与地球物理研究所
通讯作者Xu, Yonghang
作者单位1.State Ocean Adm, Open Lab Ocean & Coast Environm Geol, Inst Oceanog 3, Xiamen, Peoples R China
2.Fujian Inst Oceanog, Fujian Prov Key Lab Coast & Isl Management Techno, Xiamen, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Xu, Yonghang,Sun, Qinqin,Yi, Liang,et al. Detrital Zircons U-Pb Age and Hf Isotope from the Western Side of the Taiwan Strait: Implications for Sediment Provenance and Crustal Evolution of the Northeast Cathaysia Block[J]. TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES,2014,25(4):505-535.
APA Xu, Yonghang.,Sun, Qinqin.,Yi, Liang.,Yin, Xijie.,Wang, Aijun.,...&Chen, Jian.(2014).Detrital Zircons U-Pb Age and Hf Isotope from the Western Side of the Taiwan Strait: Implications for Sediment Provenance and Crustal Evolution of the Northeast Cathaysia Block.TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES,25(4),505-535.
MLA Xu, Yonghang,et al."Detrital Zircons U-Pb Age and Hf Isotope from the Western Side of the Taiwan Strait: Implications for Sediment Provenance and Crustal Evolution of the Northeast Cathaysia Block".TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES 25.4(2014):505-535.

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来源：地质与地球物理研究所

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