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Crustal growth as revealed by integrated U–Pb and Lu–Hf isotope analyses of detrital zircons from the Ganjiang River, southeastern China

Published online by Cambridge University Press:  14 November 2019

Andong Wang Open the ORCID record for Andong Wang [Opens in a new window] ,
Xiaocong Li ,
Xianwen Luo ,
M. Santosh ,
Yurong Cui ,
Quanzhong Li ,
Dongrong Lai ,
Jianjun Wan  and
Xuefen Zhang
Andong Wang*
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang330013, China College of Earth Sciences, East China University of Technology, Nanchang330013, China
Xiaocong Li
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang330013, China College of Earth Sciences, East China University of Technology, Nanchang330013, China
Xianwen Luo
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang330013, China College of Earth Sciences, East China University of Technology, Nanchang330013, China
M. Santosh
Affiliation:
School of Earth Science and Resources, China University of Geosciences, Beijing100083, China
Yurong Cui
Affiliation:
Tianjin Institute of Geology and Mineral Resources, China Geological Survey, Tianjin300170, China
Quanzhong Li
Affiliation:
School of Resources and Environmental Engineering, Hefei University of Technology, Hefei230009, China
Dongrong Lai
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang330013, China
Jianjun Wan
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang330013, China College of Earth Sciences, East China University of Technology, Nanchang330013, China
Xuefen Zhang
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang330013, China College of Earth Sciences, East China University of Technology, Nanchang330013, China
*
Author for correspondence: Andong Wang, Email: adw008@mail.ustc.edu.cn
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Abstract

The Ganjiang River, one of eight major tributaries of the Yangtze River, located in the western hinterland of the Cathaysia Block, SE China, has a length of 823 km and a drainage area of 82 809 km2, whose detrital zircons provide a valuable means to trace sediment provenances of the river and explore the crustal growth and evolution of the Cathaysia Block. In the current study, 389 concordia zircon U–Pb age spots and rare earth element (REE) contents, in combination with 201 Lu–Hf isotope analyses, have been determined. Oscillatory zoning, high Th/U ratios and REE distribution patterns indicate that most detrital zircon grains are of magmatic origin. The age can be further divided into seven groups: 130–185 Ma with a peak at 153 Ma (7 %); 217–379 Ma with a peak at 224 Ma (16 %); 390–494 Ma with a peak at 424 Ma (37 %); 500–698 Ma with a peak at 624 Ma (5 %); 716–897 Ma with a peak at 812 Ma (10 %); 902–1191 Ma with a peak at 976 Ma (13 %); and 2232–2614 Ma with a peak at 2471 Ma (5 %). The sources of almost all the zircon age groups can be found from the exposed rocks. In particular, Yanshanian, Hercynian to Indosinian, Pan-African, Grenvillian and Palaeoproterozoic–Archaean zircons can be mainly sourced from the northern Guangdong – southern Jiangxi – western Fujian region, while Caledonian zircons come from southern and central Jiangxi, and Jinningian zircons are from central and northern Jiangxi. Most determined zircon grains exhibit negative εHf(t) values and TDM2 ages of 797 to 4016 Ma with a wide peak at 1500–2100 Ma and a keen peak at 1824 Ma, suggesting that most zircons are sourced from the reworked ancient crustal materials or crust–mantle mixing. The zircon Hf model age cumulative probability diagram shows that rapid crustal growth took place at the Palaeo- to Mesoproterozoic and that about 90 % of the crust of the Cathaysia Block was formed before 1.5 Ga.

Keywords

Ganjiang RiverCathaysia Blockdetrital zirconU–Pb age spectracrustal growth
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 4 , April 2020 , pp. 666 - 676
Copyright
© Cambridge University Press 2019

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References

Alizai, A, Carter, A, Clift, PD, Vanlaningham, S, Williams, JC and Kumar, R (2011) Sediment provenance, reworking and transport processes in the Indus River by U–Pb dating of detrital zircon grains. Global and Planetary Change 76, 33–55.CrossRefGoogle Scholar
Belousova, EA, Kostitsyn, YA, Griffin, WL, Begg, GC, O’Reilly, SY and Pearson, NJ (2010) The growth of the continental crust: constraints from zircon Hf-isotope data. Lithos 119, 457–66.CrossRefGoogle Scholar
Blichert-Toft, J, Gleason, JD, Télouk, P and Albarède, F (1997) The Lu–Hf isotope geochemistry of shergottites and the evolution of the Martian mantle–crust system. Earth and Planetary Science Letters 148, 243–58.CrossRefGoogle Scholar
Cawood, PA, Wang, Y, Xu, Y and Zhao, G (2013) Locating South China in Rodinia and Gondwana: a fragment of great India lithosphere? Geology 41, 903–6.CrossRefGoogle Scholar
Chen, JF and Jahn, BM (1998) Crustal evolution of southeastern China: Nd and Sr isotopic evidence. Tectonophysics 284, 101–33.CrossRefGoogle Scholar
Cheng, ZJ (2003) Tracing the Headstream of the Ganjiang River. Nanchang: Jiangxi Scientific and Technological Press, 144 pp. (in Chinese).Google Scholar
Choi, T, Yong, IL and Orihashi, Y (2016) Crustal growth history of the Korean Peninsula: constraints from detrital zircon ages in modern river sediments. Geoscience Frontiers (English version) 7, 707–14.CrossRefGoogle Scholar
Condie, KC (2014) Growth of continental crust: a balance between preservation and recycling. Mineralogical Magazine 78, 623–37.CrossRefGoogle Scholar
Condie, KC and Aster, RC (2010) Episodic zircon age spectra of orogenic granitoids: the supercontinent connection and continental growth. Precambrian Research 180, 227–36.CrossRefGoogle Scholar
Condie, KC, Belousova, E, Griffin, WL and Sircombe, KN (2009) Granitoid events in space and time: constraints from igneous and detrital zircon age spectra. Gondwana Research 15, 228–42.CrossRefGoogle Scholar
Corfu, F, Hanchar, JM, Hoskin, PWO and Kinny, P (2003) Atlas of zircon textures. Reviews in Mineralogy and Geochemistry 53, 469–500.CrossRefGoogle Scholar
Gao, WL, Wang, ZX and Li, CL (2017) Triassic magmatism in the eastern part of the South China Block: geochronological and petrogenetic constraints from Indosinian granites. Geoscience Frontiers 8, 445–56.CrossRefGoogle Scholar
Gilder, SA, Gill, J, Coe, RS, Zhao, XX, Liu, ZW, Wang, GX, Yuan, KL, Liu, WL, Kuang, GD and Wu, HR (1996) Isotopic and paleomagnetic constraints on the Mesozoic tectonic evolution of south China. Journal of Geophysical Research Atmospheres 1011, 16137–54.CrossRefGoogle Scholar
Grabau, AW (1924) Stratigraphy of China. Part I, Paleozoic and Older. Peking: Geological Survey of Agriculture and Commerce, 528 pp.Google Scholar
Griffin, WL, Pearson, NJ, Belousova, E, Jackson, SE, van Achterbergh, E, O’Reilly, SY and Shee, SR (2000) The Hf isotope composition of cratonic mantle: LA-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochimica et Cosmochimica Acta 64, 133–47.CrossRefGoogle Scholar
Griffin, WL, Wang, X, Jackson, SE, Pearson, NJ, O’Reilly, SY, Xu, XS and Zhou, XM (2002) Zircon chemistry and magma mixing, SE China: in-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes. Lithos 61, 237–69.CrossRefGoogle Scholar
Guo, CL, Chen, YC, Lin, ZY, Lou, FS and Zeng, ZL (2011) SHRIMP zircon U–Pb dating, geochemistry and zircon Hf isotopic characteristics of granitoids in Keshuling granites, Jiangxi Province and their genetic analysis. Acta Petrologica et Mineralogica 30, 567–80 (in Chinese with English abstract).Google Scholar
Guo, F, Fan, W, Li, C, Zhao, L, Li, H and Yang, J (2012) Multi-stage crust-mantle interaction in SE China: temporal, thermal and compositional constraints from the Mesozoic felsic volcanic rocks in eastern Guangdong-Fujian provinces. Lithos 150, 62–84.CrossRefGoogle Scholar
Guo, LZ, Shi, YS, Lu, HF, Ma, RS, Dong, HG and Yang, SF (1989) The pre-Devonian tectonic patterns and evolution of South China. Journal of Asian Earth Sciences 3, 87–93.Google Scholar
He, MY, Zheng, HB and Jia, J (2013) Detrital zircons U–Pb dating and Hf isotope of modern sediments in the Yangtze River: implications for the sediment provenance. Quaternary Sciences 33, 656–70 (in Chinese with English abstract).Google Scholar
Huang, HQ, Li, XH, Li, ZX and Li, WX (2015) Formation of the Jurassic South China Large Granitic Province: insights from the genesis of the Jiufeng pluton. Chemical Geology 401, 43–58.CrossRefGoogle Scholar
Iizuka, T, Hirata, T, Komiya, T, Rino, S, Katayama, I, Motoki, A and Maruyama, S (2005) U–Pb and Lu–Hf isotope systematics of zircons from the Mississippi River sand: implications for reworking and growth of continental crust. Geology 33, 485–8.CrossRefGoogle Scholar
Iizuka, T, Komiya, T, Rino, S, Maruyama, S and Hirata, T (2010) Detrital zircon evidence for Hf isotopic evolution of granitoid crust and continental growth. Geochimica et Cosmochimica Acta 74, 2450–72.CrossRefGoogle Scholar
Li, LM, Sun, M, Wang, YJ, Xing, GF, Zhao, GC, He, YH, He, KJ and Zhang, AM (2011) U–Pb and Hf isotopic study of detrital zircons from the meta-sedimentary rocks in central Jiangxi Province, South China: implications for the Neoproterozoic tectonic evolution of South China Block. Journal of Asian Earth Sciences 41, 44–55.CrossRefGoogle Scholar
Li, XH (1997) Timing of the Cathaysia Block formation: constraints from SHRIMP U–Pb zircon geochronology. Episodes 20, 188–92.CrossRefGoogle Scholar
Li, XH, Chen, ZG, Liu, DY and Li, WX (2003a) Jurassic gabbro-granite-syenite suites from Southern Jiangxi Province, SE China: age, origin, and tectonic significance. International Geology Review 45, 898–921.CrossRefGoogle Scholar
Li, XH, Li, WX and He, B (2012) Building of the South China Block and its relevance to assembly and breakup of Rodinia supercontinent: observations, interpretations and tests. Bulletin of Mineralogy, Petrology and Geochemistry 31, 543–59 (in Chinese with English abstract).Google Scholar
Li, XH, Li, ZX, Ge, WC, Zhou, HW, Li, WX, Liu, Y and Michanl, TDW (2003b) Neoproterozoic granitoids in South China: crustal melting above a mantle plume at ca. 825 Ma? Precambrian Research 122, 45–83.CrossRefGoogle Scholar
Li, XH, Long, WG, Li, QL, Liu, Y, Zheng, YF, Yang, YH, Chamberlain, KR, Wan, DF, Guo, CH, Wang, XC and Tao, H (2010b) Penglai zircon megacrysts: a potential new working reference material for microbeam determination of Hf–O isotopes and U–Pb age. Geostandards & Geoanalytical Research 34, 117–34.CrossRefGoogle Scholar
Li, XY, Zheng, JP, Xiong, Q, Zhou, X and Xiang, L (2018) Triassic rejuvenation of unexposed Archean-Paleoproterozoic deep crust beneath the Western Cathaysia Block, South China. Tectonophysics 724–725, 65–79.CrossRefGoogle Scholar
Li, ZX and Li, XH (2007) Formation of the 1300 km-wide intra-continental orogen and post-orogenic magmatic province in Mesozoic South China: a flat-slab subduction model. Geology 35, 179–82.CrossRefGoogle Scholar
Li, ZX, Li, XH, Wartho, JA, Clark, C, Li, WX, Zhang, CL and Bao, CM (2010a) Magmatic and metamorphic events during the early Paleozoic Wuyi-Yunkai orogeny, southeastern South China: new age constraints and pressure-temperature conditions. GSA Bulletin 122, 772–93.CrossRefGoogle Scholar
Link, PK, Fanning, CM and Beranek, LP (2005) Reliability and longitudinal change of detrital-zircon age spectra in the Snake River system, Idaho and Wyoming: an example of reproducing the bumpy barcode. Sedimentary Geology 182, 101–42.CrossRefGoogle Scholar
Liu, Q, Yu, JH, O’Reilly, SY, Zhou, MF, Griffin, WL, Wang, LJ and Cui, X (2014) Origin and geological significance of Paleoproterozoic granites in the northeastern Cathaysia Block, South China. Precambrian Research 248, 72–95.CrossRefGoogle Scholar
Liu, XC, Wu, YB, Fisher, CM, Hanchar, JM, Beranek, L, Gao, S and Wang, H (2017) Tracing crustal evolution by U-Th-Pb, Sm-Nd, and Lu–Hf isotopes in detrital monazite and zircon from modern rivers. Geology 45, 103–6.CrossRefGoogle Scholar
Liu, YS, Gao, S, Hu, ZC, Gao, CG, Zong, KP and Wang, DB (2010a) Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U–Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology 51, 537–71.CrossRefGoogle Scholar
Liu, YS, Hu, ZC, Zong, KP, Gao, CG, Gao, S, Xu, J and Chen, HH (2010b) Reappraisement and refinement of zircon U–Pb isotope and trace element analyses by LA-ICP-MS. Chinese Science Bulletin 55, 1535–46.CrossRefGoogle Scholar
Lou, FS, Shen, WZ, Wang, DZ, Shu, LS, Wu, FJ, Zhang, FR and Yu, JH (2005) Zircon U–Pb isotopic chronology of the Wugongshan dome compound granite in Jiangxi Province. Acta Geologica Sinica 79, 636–44 (In Chinese with English abstract).Google Scholar
Ludwig, KR (2003) User’s Manual for Isoplot 3.00, vol. 4. Berkeley, California: Berkeley Geochronology Center Special Publication, 71 pp.Google Scholar
Luo, ZG, Wang, YJ, Zhang, FF, Zhang, AM and Zhang, YZ (2010) LA-ICPMS zircon U–Pb dating for Baimashan and Jintan Indosinian granitic plutons and its petrogenetic implications. Geotectonica et Metallogenia 34, 282–90 (in Chinese with English abstract).Google Scholar
Rino, S, Komiya, T, Windley, BF, Katayama, I, Motoki, A and Hirata, T (2004) Major episodic increases of continental crustal growth determined from zircon ages of river sands: implications for mantle overturns in the early Precambrian. Physics of the Earth & Planetary Interiors 146, 369–94.CrossRefGoogle Scholar
Safonova, I, Maruyama, S, Hirata, T, Kon, Y and Rino, S (2010) LA-ICP-MS U–Pb ages of detrital zircons from Russia largest rivers: implications for major granitoid events in Eurasia and global episodes of supercontinent formation. Journal of Geodynamics 50, 134–53.CrossRefGoogle Scholar
Shen, WZ, Zhang, FR, Shu, LS, Wang, LJ and Xiang, L (2008) Formation age, geochemical characteristics of the Ninggang granite body in Jiangxi Province and its tectonic significance. Acta Petrologica Sinica 24, 2244–54 (In Chinese with English abstract).Google Scholar
Shu, LS, Deng, P, Yu, JH, Wang, YB and Jiang, SY (2008) The age and tectonic environment of the rhyolitic rocks on the western side of Wuyi Mountain, South China. Science China: Earth Sciences 51, 1053–63.CrossRefGoogle Scholar
Söderlund, U, Patchett, PJ, Vervoort, JD and Isachsen, CE (2004) The 176Lu decay constant determined by Lu–Hf and U–Pb isotope systematics of Precambrian mafic intrusions. Earth and Planetary Science Letters 219, 311–24.CrossRefGoogle Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and process. In Magmatism in the Ocean Basins. (eds Saunders, AD and Norry, MJ), pp. 313–45. Geological Society of London, Special Publication no. 42.Google Scholar
Sun, T (2006) A new map showing the distribution of granites in South China and its explanatory notes. Geological Bulletin of China 25, 332–5 (in Chinese with English abstract).Google Scholar
Tao, JH, Li, WX, Wyman, DA, Wang, AD and Xu, ZT (2018) Petrogenesis of Triassic granite from the Jintan pluton in Central Jiangxi Province, South China: implication for uranium enrichment. Lithos 320–321, 62–74.CrossRefGoogle Scholar
Wang, CY, Campbell, IH, Allen, CM, Williams, IS and Eggins, SM (2009) Rate of growth of the preserved North American continental crust: evidence from Hf and O isotopes in Mississippi detrital zircons. Geochimica et Cosmochimica Acta 73, 712–28.CrossRefGoogle Scholar
Wang, CY, Campbell, IH, Stepanov, AS, Allen, CM and Burtsev, IN (2011) Growth rate of the preserved continental crust: II. Constraints from Hf and O isotopes in detrital zircons from Greater Russian Rivers. Geochimica et Cosmochimica Acta 75, 1308–45.CrossRefGoogle Scholar
Wang, LJ, Yu, JH, O’Reilly, SY, Griffin, WL, Sun, T, Wei, ZY, Jiang, SY and Shu, LS (2008) Grenvillian orogeny in the Southern Cathaysia Block: constraints from U–Pb ages and Lu–Hf isotopes in zircon from metamorphic basement. Chinese Science Bulletin 53, 3037–50.Google Scholar
Wang, XL, Yu, JH, Shu, XJ, Tang, CH and Xing, GF (2013) U–Pb geochronology of detrital zircons from the parametamorphic rocks of the Zhoutan Group, central Jiangxi Province. Acta Petrologica Sinica 29, 801–11 (in Chinese with English abstract).Google Scholar
Wang, XL, Zhao, GC, Zhou, JC, Liu, YS, Hu, J (2008) Geochronology and Hf isotopes of zircon from volcanic rocks of the Shuangqiaoshan Group, South China: implications for the Neoproterozoic tectonic evolution of the eastern Jiangnan orogen. Gondwana Research 14, 355–67.CrossRefGoogle Scholar
Wang, YJ, Zhang, FF, Fan, WM, Zhang, GW, Chen, SY, Cawood, PA and Zhang, AM (2010) Tectonic setting of the South China Block in the early Paleozoic: resolving intracontinental and ocean closure models from detrital zircon U–Pb geochronology. Tectonics 29, 1–70.CrossRefGoogle Scholar
Wang, YJ, Zhang, YZ, Fan, WM, Geng, HY and Zou, HP (2014) Early Neoproterozoic accretionary assemblage in the Cathaysia Block: geochronological, Lu–Hf isotopic and geochemical evidence from granitoid gneisses. Precambrian Research 249, 144–61.CrossRefGoogle Scholar
Wu, FY, Yang, YH, Xie, LW, Yang, JH and Xu, P (2006) Hf isotopic compositions of the standard zircons and baddeleyites in U–Pb geochronology. Chemical Geology 234, 105–26.CrossRefGoogle Scholar
Wu, YB and Zheng, YF (2004) Genesis of zircon and its constraints on interpretation of U–Pb age. Chinese Science Bulletin 49, 1554–69.CrossRefGoogle Scholar
Xiang, L and Shu, LS (2010) Pre-Devonian tectonic evolution of the eastern South China Block: geochronological evidence from detrital zircons. Science China Earth Sciences 53, 1427–44.CrossRefGoogle Scholar
Xu, XS, O’Reilly, SY, Griffin, WL, Deng, P and Pearson, NJ (2005) Relict Proterozoic basement in the Nanling Mountains (SE China) and its tectonothermal overprinting. Tectonics 24, 187–200.CrossRefGoogle Scholar
Xu, XS, O’Reilly, SY, Griffin, WL, Wang, XL, Pearson, NJ and He, ZY (2007) The crust of Cathaysia: age, assembly and reworking of two terranes. Precambrian Research 158, 51–78.CrossRefGoogle Scholar
Xu, Y, Wang, CY and Zhao, T (2016), Using detrital zircons from river sands to constrain major tectono-thermal events of the Cathaysia block, SE China. Journal of Asian Earth Sciences 124, 1–13.CrossRefGoogle Scholar
Yang, J, Gao, S, Chen, C, Tang, YG, Yuan, HL, Gong, HJ, Xie, SW and Wang, JQ (2009) Episodic crustal growth of North China as revealed by U–Pb age and Hf isotopes of detrital zircons from modern rivers. Geochimica et Cosmochimica Acta 73, 2660–73.CrossRefGoogle Scholar
Yang, SY, Zhang, F and Wang, ZB (2012) Grain size distribution and age population of detrital zircons from the Changjiang (Yangtze) River system, China. Chemical Geology s296–297, 26–38.CrossRefGoogle Scholar
Yao, JL, Shu, LS and Santosh, M (2011) Detrital zircon U–Pb geochronology, Hf-isotopes and geochemistry: new clues for the Precambrian crustal evolution of Cathaysia Block, South China. Gondwana Research 20, 553–67.CrossRefGoogle Scholar
Yu, JH, O’Reilly, SY, Wang, LJ, Griffin, WL, Jiang, SY, Wang, RC and Xu, XS (2007) Finding of ancient materials in Cathaysia and implication for the formation of Precambrian crust. Science Bulletin 52, 13–22.CrossRefGoogle Scholar
Yu, JH, O’Reilly, SY, Wang, LJ, Griffin, WL, Zhang, M, Wang, RS, Jiang, SY and Shu, LS (2008) Where was South China in the Rodinia supercontinent?: evidence from U–Pb geochronology and Hf isotopes of detrital zircons. Precambrian Research 164, 1–15.CrossRefGoogle Scholar
Yu, JH, O’Reilly, SY, Zhou, MF, Griffin, WL and Wang, LJ (2012a) U–Pb geochronology and Hf–Nd isotopic geochemistry of the Badu Complex, Southeastern China: implications for the Precambrian crustal evolution and paleogeography of the Cathaysia Block. Precambrian Research s222–223, 424–49.CrossRefGoogle Scholar
Yu, Y, Chen, ZY, Chen, ZH, Hou, KJ, Zhao, Z, Xu, JX, Zhang, JJ and Zeng, ZL (2012b) Zircon U–Pb dating and mineralization prospective of the Triassic Qingxi Pluton in Southern Jiangxi Province. Geotectonica et Metallogenia 36, 413–21.Google Scholar
Yuan, HL, Gao, S, Dai, MN, Zong, CL, Günther, D, Fontaine, GH, Liu, XM and Diwu, CR (2008) Simultaneous determinations of U–Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS. Chemical Geology 247, 100–18.CrossRefGoogle Scholar
Zhang, AM, Wang, YJ, Fan, WM, Zhang, YZ and Yang, J (2012) Earliest Neoproterozoic (ca.1.0 Ga) arc-back-arc basin nature along the northern Yunkai Domain of the Cathaysia Block: geochronological and geochemical evidence from the metabasite. Precambrian Research 220–221, 217–33.CrossRefGoogle Scholar
Zhang, FF, Wang, YJ, Fan, WM, Zhang, AM and Zhang, YZ (2010) LA-ICPMS zircon U–Pb geochronology of late Early Paleozoic granites in eastern Hunan and western Jiangxi provinces, South China. Geochimica 39, 414–26 (In Chinese with English abstract).Google Scholar
Zhang, FR, Shu, LS, Wang, DZ, Shen, WZ, Yu, JH, and Xie, L (2010) Study on geochronological, geochemical features and genesis of the Fufang granitic pluton in the Jiangxi Province, South China. Geological Journal of China Universities 16, 161–76 (In Chinese with English abstract).Google Scholar
Zhao, GC (2015) Jiangnan Orogen in South China: developing from divergent double subduction. Gondwana Research 27, 1173–80.CrossRefGoogle Scholar
Zhao, GC and Cawood, PA (2012) Precambrian geology of China. Precambrian Research s222–223, 13–54.CrossRefGoogle Scholar
Zheng, JP, Griffin, WL, Tang, HY, Zhang, ZH, Su, YP and Liu, GL (2008) Archean basement similar to the North China and Yangtze continents may be existed beneath the western Cathaysia. Geological Journal of China Universities 14, 549–57 (in Chinese with English abstract).Google Scholar
Zheng, YF, Wu, YB, Zhao, ZF, Zhang, SB, Xu, P and Wu, FY (2005) Metamorphic effect on zircon Lu–Hf and U–Pb isotope systems in ultrahigh-pressure eclogite-facies metagranite and metabasite. Earth and Planetary Science Letters 240, 378–400.CrossRefGoogle Scholar
Zheng, YF and Zhang, SB (2007) Formation and evolution of Precambrian continental crust in South China. Science Bulletin 52, 1–12.CrossRefGoogle Scholar
Zhong, YF, Ma, CQ, Liu, L, Zhao, JH, Zheng, JP, Nong, JN and Zhang, ZJ (2014) Ordovician appinites in the Wugongshan Domain of the Cathaysia Block, South China: geochronological and geochemical evidence for intrusion into a local extensional zone within an intracontinental regime. Lithos s198–199, 202–16.CrossRefGoogle Scholar
Zhou, XM (2007) Petrogenesis of Late Mesozoic Granites in Nanling Region and Their Lithospheric Dynamics Implications. Beijing: Science Press, 691 pp. (in Chinese).Google Scholar
Zhou, XM and Li, WX (2000) Origin of Late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas. Tectonophysics 326, 269–87.CrossRefGoogle Scholar
Zhou, XM, Sun, T, Shen, WZ, Shu, LS and Niu, YL (2006) Petrogenesis of Mesozoic granitoids and volcanic rocks in South China: a response to tectonic evolution. Episodes 29, 26–33.CrossRefGoogle Scholar
Zhou, ZM, Xie, CF, Sun, WL, Guo, FS, Zhou, WP, Liu, LQ and Liu, W (2015) Zircon LA-ICP-MS U–Pb dating of the Xiankou Granitoid in Le’an county, Jiangxi Province and its geological significance. Acta Geologica Sinica 89, 83–98 (In Chinese with English abstract).Google Scholar
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