Hostname: page-component-78c5997874-s2hrs Total loading time: 0 Render date: 2024-11-19T11:54:42.139Z Has data issue: false hasContentIssue false
  • English
  • Français

Crustal growth event in the Cathaysia Block at 2.5 Ga: evidence from chronology and geochemistry of captured zircons in Jurassic acidic dykes

Published online by Cambridge University Press:  20 July 2020

Shuang-Lian Li ,
Jian-Qing Lai ,
Wen-Zhou Xiao Open the ORCID record for Wen-Zhou Xiao [Opens in a new window] ,
Elena A. Belousova ,
Tracy Rushmer ,
Le-Jun Zhang ,
Quan Ou Open the ORCID record for Quan Ou [Opens in a new window]  and
Chao-Yun Liu
Shuang-Lian Li
Affiliation:
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha410083, China School of Geosciences and Info-Physics, Central South University, Changsha410083, China
Jian-Qing Lai*
Affiliation:
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha410083, China School of Geosciences and Info-Physics, Central South University, Changsha410083, China
Wen-Zhou Xiao*
Affiliation:
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha410083, China School of Geosciences and Info-Physics, Central South University, Changsha410083, China
Elena A. Belousova
Affiliation:
ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia
Tracy Rushmer
Affiliation:
ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia
Le-Jun Zhang
Affiliation:
Centre of Excellence in Ore Deposits (CODES), University of Tasmania, Private Bag 79, Hobart, Australia
Quan Ou
Affiliation:
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha410083, China School of Geosciences and Info-Physics, Central South University, Changsha410083, China State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China
Chao-Yun Liu
Affiliation:
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha410083, China School of Geosciences and Info-Physics, Central South University, Changsha410083, China
*
Authors for correspondence: Jian-Qing Lai, Email: ljq@csu.edu.cn and Wen-Zhou Xiao, Email: lilzhou@csu.edu.cn
Authors for correspondence: Jian-Qing Lai, Email: ljq@csu.edu.cn and Wen-Zhou Xiao, Email: lilzhou@csu.edu.cn
Get access Rights & Permissions [Opens in a new window]

Abstract

Six acidic dykes were discovered surrounding the Laiziling pluton, Xianghualing area, in the western Cathaysia Block, South China. A number of captured zircons are found in two of these acidic dykes. By detailed U–Pb dating, Lu–Hf isotopes and trace-element analysis, we find that these zircons have ages clustered at c. 2.5 Ga. Two acidic dyke samples yielded upper intersection point 206U/238Pb ages of 2505 ± 42 Ma and 2533 ± 22 Ma, and weighted mean 207Pb/206Pb ages of 2500 ± 30 Ma and 2535 ± 16 Ma. The majority of these zircons have high (Sm/La)N, Th/U and low Ce/Ce* ratios, indicating a magmatic origin, but some grains were altered by later hydrothermal fluid. Additionally, the magmatic zircons have high Y, U, heavy rare earth element, Nb and Ta contents, indicating that their host rocks were mainly mafic rocks or trondhjemite–tonalite–granodiorite rock series. Equally, their moderate Y, Yb, Th, Gd and Er contents also indicate that a mafic source formed in a continental volcanic-arc environment. These zircons have positive ϵHf(t) values (2.5–6.9) close to zircons from the depleted mantle, with TDM (2565–2741 Ma) and TDM2 (2608–2864 Ma) ages close to their formation ages, indicating that these zircons originated directly from depleted mantle magma, or juvenile crust derived from the depleted mantle in a very short period. We therefore infer that the Cathaysia Block experienced a crustal growth event at c. 2.5 Ga.

Keywords

acidic dykecaptured zircondetrital zirconCathaysia Block
Type
Original Article
Information
Geological Magazine , Volume 158 , Issue 4 , April 2021 , pp. 567 - 582
Copyright
© The Author(s), 2020. Published by Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Andersen, T (2002) Correction of common lead in U–Pb analyses that do not report 204Pb. Chemical Geology 192, 59–79.CrossRefGoogle Scholar
Belousova, E, Griffin, W, O’Reilly, SY and Fisher, N (2002) Igneous zircon: trace element composition as an indicator of source rock type. Contributions to Mineralogy and Petrology 143(5), 602–22.CrossRefGoogle Scholar
Carley, TL, Miller, CF, Wooden, JL, Padilla, AJ, Schmitt, AK, Economos, RC, Bindeman, IN and Jordan, BT (2014) Iceland is not a magmatic analog for the Hadean: evidence from the zircon record. Earth and Planetary Science Letters 405, 85–97.CrossRefGoogle Scholar
Cawood, PA, Zhao, GC, Yao, JL, Wang, W, Xu, YJ and Wang, YJ (2018) Reconstructing South China in Phanerozoic and Precambrian supercontinents. Earth-Science Reviews 186, 173–94.CrossRefGoogle Scholar
Chen, Y, Wu, TR, Gan, L, Zhang, Z and Fu, B (2019) Provenance of the early to mid-Paleozoic sediments in the northern Alxa area: implications for tectonic evolution of the southwestern Central Asian Orogenic Belt. Gondwana Research 67, 115–30.CrossRefGoogle Scholar
Edmund, ZC (2000) Geology and tectonics of the Songpan-Ganzi fold belt, southwestern china. International Geology Review 42(9), 813–31.Google Scholar
El-Bialy, MZ and Ali, KA (2013) Zircon trace element geochemical constraints on the evolution of the Ediacaran (600-614Ma) post-collisional Dokhan Volcanics and Younger Granites of SE Sinai, NE Arabian–Nubian Shield. Chemical Geology 360–361, 54–73.CrossRefGoogle Scholar
Enkelmann, E, Weislogel, A, Ratschbacher, L, Eide, E, Renno, A and Wooden, J (2007) How was the Triassic Songpan-Ganzi basin filled? A provenance study. Tectonics 26(4), 1–24.CrossRefGoogle Scholar
Ge, RF, Wilde, SA, Nemchin, AA, Whitehouse, MJ, Bellucci, JJ and Erickson, TM (2019) Mechanisms and consequences of intra-crystalline enrichment of ancient radiogenic Pb in detrital Hadean zircons from the Jack Hills,Western Australia. Earth and Planetary Science Letters 517, 38–49.CrossRefGoogle Scholar
Grimes, CB, John, BE, Kelemen, PN, Mazdab, FK, Wooden, JL, Cheadle, MJ, Hanghoj, K and Schwartz, JJ (2007) Trace element chemistry of zircons from oceanic crust: a method for distinguishing detrital zircon provenance. Geology 35(7), 643–6.CrossRefGoogle Scholar
Grimes, CB, Wooden, JL, Cheadle, MJ and John, BE (2015) “Fingerprinting” tectono-magmatic provenance using trace elements in igneous zircon. Contributions to Mineralogy and Petrology 170, 1–26.CrossRefGoogle Scholar
Hacker, BR, Ratschbacher, L and Liou, JG (2004) Subduction, collision and exhumation in the ultrahigh-pressure Qinling-Ddabie orogen. In Aspects of the Tectonic Evolution of China (eds Malpas, J, Fletcher, CJN, Ali, JR and Aitchison, JC), pp. 157–75. Geological Society of London, Special Publication no. 226.Google Scholar
Hoskin, PWO (2005) Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia. Geochimica et Cosmochimica Acta 69, 637–48.CrossRefGoogle Scholar
Hoskin, PWO, Kinny, PD, Wyborn, D and Chappell, BW (2000) Identifying accessory mineral saturation during differentiation in granitoid magmas: an integrated approach. Journal of Petrology 41(9), 1365–96.CrossRefGoogle Scholar
Hoskin, PWO and Schaltegger, U (2003) The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry 53, 27–62.CrossRefGoogle Scholar
Hu, Z, Liu, Y, Chen, L, Zhou, L, Li, M and Zong, K (2011) Contrasting matrix induced elemental fractionation IN NIST SRM and rock glasses during laser ablation ICP-MS analysis at high spatial resolution. Journal of Analytical Atomic Spectrometry 26(2), 425–30.CrossRefGoogle Scholar
Huang, FF, Wang, RC, Xie, L, Zhu, JC, Erdmann, S, Che, XD and Zhang, RQ (2015) Differentiated rare-element mineralization in an ongonite-topazite composite dike at the Xianghualing tin district, Southern China: an electron-microprobe study on the evolution from niobium-tantalum-oxides to cassiterite. Ore Geology Reviews 65, 761–78.CrossRefGoogle Scholar
Lai, SH (2014) Research on mineralization of the Xianghualing tin polymetallic deposit, Hunan Province, China. Ph.D. thesis, China University of Geosciences, Beijing. Published thesis (in Chinese with English abstract).Google Scholar
Li, H, Watanabe, K and Yonezu, K (2014a) Zircon morphology, geochronology and trace element geochemistry of the granites from the Huangshaping polymetallic deposit, South China: implications for the magmatic evolution and mineralization processes. Ore Geology Reviews 60, 14–35.CrossRefGoogle Scholar
Li, H, Wu, J, Evans, NJ, Jiang, W and Zhou, Z (2018a) Zircon geochronology and geochemistry of the Xianghualing A-type granitic rocks: insights into multi-stage Sn-polymetallic mineralization in South China. Lithos 312–313, 1–20.CrossRefGoogle Scholar
Li, XH, Li, ZX and Li, WX (2014b) Detrital zircon U-Pb age and Hf isotope constrains on the generation and reworking of Precambrian continental crust in the Cathaysia Block, South China: a synthesis. Gondwana Research 25, 1202–15.CrossRefGoogle Scholar
Li, XY, Zheng, JP, Xiong, Q, Zhou, X and Xiang, L (2018b) Triassic rejuvenation of unexposed Archean-Paleoproterozoic deep crust beneath the western Cathaysia block, South China. Tectonophysics 724–725, 65–79.CrossRefGoogle Scholar
Liu, J, Liu, F, Ding, Z, Liu, C, Yang, H, Liu, P, Wang, F and Meng, E (2013) The growth, reworking and metamorphism of early Precambrian crust in the Jiaobei terrane, the North China Craton: constraints from U-Th-Pb and Lu-Hf isotopic systematics, and REE concentrations of zircon from Archean granitoid gneisses. Precambrian Research 224, 287–303.CrossRefGoogle Scholar
Liu, Y, Gao, S, Hu, Z, Gao, C, Zong, K and Wang, D (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(1–2): 537–71.CrossRefGoogle Scholar
Liu, Y, Lai, JQ, Xiao, WZ, Jeffrey, MD, Du, RJ, Li, SL, Liu, CY, Wen, CH and Yu, XH (2019) Petrogenesis and mineralization significance of two-stage A-type granites in Jiuyishan, South China: Constraints from whole-rock geochemistry, mineral composition and zircon U-Pb-Hf isotopes. Acta Geologica Sinica (English Edition) 93(4): 874–900.CrossRefGoogle Scholar
Liu, YS, Hu, ZC, Zong, KQ, Gao, CG, Gao, S and Xu, J (2010b) Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Science Bulletin 55(15), 1535–46.CrossRefGoogle Scholar
Lu, J, Zheng, J, Griffin, W L and Yu, C (2013) Petrology and geochemistry of peridotite xenoliths from the Lianshan region: nature and evolution of lithospheric mantle beneath the lower Yangtze block. Gondwana Research 23(1), 161–75.CrossRefGoogle Scholar
Ludwig, KR (2003) User’s Manual for Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley: Berkeley Geochronology Center, Special Publication no. 4.Google Scholar
Ma, Q, Xu, YG, Huang, XL, Zheng, JP, Ping, XQ and Xia, XP (2020) Eoarchean to Paleoproterozoic crustal evolution in the North China Craton: evidence from U-Pb and Hf-O isotopes of zircons from deep-crustal xenoliths. Geochimica et Cosmochimica Acta 278, 94–109.CrossRefGoogle Scholar
O’Reilly, SY and Griffin, WL (2013) Moho vs crust-mantle boundary: evolution of an idea. Tectonophysics 609, 535–46.CrossRefGoogle Scholar
Pan, S, Zheng, J, Griffin, WL, Xu, Y and Li, X (2015) Nature and evolution of the lithospheric mantle beneath the eastern central Asian orogenic belt: constraints from peridotite xenoliths in the central part of the great Xing’an range, NE china. Lithos 238, 52–63.CrossRefGoogle Scholar
Qiu, RZ, Deng, JF, Cai, ZY, Zhou, S, Chang, HL and Du, SH (2002) Material sources of granite and ore in Xianghualing mult-metal orefield, Hunan Province. Mineral Deposits 21, 1017–20.Google Scholar
Schultz, B, Klemd, R and Brätz, H (2006) Host rock compositional controls on zircon trace element signatures in metabasites from the Austroalpine basement. Geochimica et Cosmochimica Acta 70, 697–710.CrossRefGoogle Scholar
Shu, XJ, Wang, XL, Sun, T, Chen, WF and Shen, WZ (2013) Crustal formation in the Nanling Range, South China craton: Hf isotope evidence of zircons from Phanerozoic granitoids. Journal of Asian Earth Sciences 74, 210–24.CrossRefGoogle Scholar
Shu, XJ, Wang, XL, Sun, T, Xu, X and Dai, MN (2011) Trace elements, U-Pb ages and Hf isotopes of zircons from Mesozoic granites in the western Nanling Range, South China: implications for petrogenesis and W-Sn mineralization. Lithos 127(3–4), 468–82.CrossRefGoogle Scholar
Sun, P, Niu, Y, Guo, P, Cui, H, Ye, L and Liu, J (2018) The evolution and ascent paths of mantle xenolith-bearing magma: observations and insights from Cenozoic basalts in southeast China. Lithos 310–311, 171–81.CrossRefGoogle Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In Magmatism in the Ocean Basins (eds Saunders, AD and Norry, MJ), pp. 313–45. Geological Society of London, Special Publication no. 42.CrossRefGoogle Scholar
Wu, FY, Liu, XC, Ji, WQ, Wang, JM and Yang, L (2017) Highly fractionated granites: recognition and research. Science China Earth Sciences 60, 1201–19 (in Chinese).CrossRefGoogle Scholar
Wu, J, Li, H, Algeo, TJ, Jiang, W and Zhou, Z (2018) Genesis of the Xianghualing Sn-Pb-Zn deposit, South China: a multi-method zircon study. Ore Geology Reviews 102, 220–39.CrossRefGoogle Scholar
Wu, Q, Cao, J, Kong, H, Shao, Y, Li, H, Xi, X and Deng, X (2016) Petrogenesis and tectonic setting of the early Mesozoic Xitian granitic pluton in the middle Qin-Hang Belt, South China: constraints from zircon U-Pb ages and bulk-rock trace element and Sr-Nd-Pb isotopic compositions. Journal of Asian Earth Sciences 128, 130–48.CrossRefGoogle Scholar
Wu, YB and Zheng, Y F (2004) Research on the zircon genetic mineralogy and constraints of its U-Pb ages. Chinese Science Bulletin 49, 1589–604 (in Chinese).CrossRefGoogle Scholar
Xia, Y, Xu, XS, Niu, YL and Liu, L (2018) Neoproterozoic amalgamation between Yangtze and Cathaysia blocks: the magmatism in various tectonic settings and continent-arc-continent collision. Precambrian Research 309, 56–87.CrossRefGoogle Scholar
Xiao, C, Shen, Y and Wei, C (2019) Petrogenesis of low Sr and high Yb A-type granitoids in the Xianghualing Sn polymetallic deposit, South China: constrains from geochronology and Sr-Nd-Pb-Hf isotopes. Minerals 9(3), 182.CrossRefGoogle Scholar
Xie, L, Wang, RC, Zhu, JC, Lu, JJ, Zhang, WL, Che, XD, Zhang, RQ and Huang, FF (2013) Felsic dykes in the metallogenic area of southern Hunan Province and their implications for mineralization and exploration. Acta Petrologica Sinica 29(12), 4261–80 (in Chinese with English abstract).Google Scholar
Xuan, Y, Yuan, S, Yuan, Y and Mi, J (2014) Zircon U-Pb age, geochemistry and petrogenesis of Jianfengling pluton in southern Hunan Province. Mineral Deopsits 33(6), 1379–90 (in Chinese with English abstract).Google Scholar
Yang, F, Santosh, M, Tsunogae, T, Tang, L and Teng, X (2017) Multiple magmatism in an evolving suprasubduction zone mantle wedge: the case of the composite mafic–ultramafic complex of Gaositai, North China Craton. Lithos 284–285, 525–44.CrossRefGoogle Scholar
Yang, L, Wu, X, Cao, J, Hu, B, Zhang, X, Gong, Y and Liu, W (2018) Geochronology, petrology, and genesis of two granitic plutons of the Xianghualing ore field in South Hunan Province: constraints from Zircon U-Pb dating, geochemistry, and Lu-Hf isotopic compositions. Minerals 8(5), 213.CrossRefGoogle Scholar
Yao, J, Shu, L 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
Yao, WH, Li, ZX, Li, WX, Su, L and Yang, JH (2015) Detrital provenance evolution of the Ediacaran-Silurian Nanhua foreland basin, South China. Gondwana Research 28, 1449–65.CrossRefGoogle Scholar
Yu, JH, O’Reilly, SY, Wang, LJ, Griffin, WL, Zhang, M, Wang, R, Jiang, S and Shu, L (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, Wang, LJ, Griffin, WL, Zhou, MF, Zhang, M and Shu, LS (2010) Components and episodic growth of Precambrian crust in the Cathaysia Block, South China: evidence from U-Pb ages and Hf isotopes of zircons in Neoproterozoic sediments. Precambrian Research 181, 97–114.CrossRefGoogle Scholar
Yu, JH, O’Reilly, SY, Zhou, MF, Griffin, WL and Wang, LJ (2012) 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 222–223, 424–49.CrossRefGoogle Scholar
Yu, JH, Wang, LJ, O’Reilly, SY, Griffin, WL, Zhang, M, Li, CZ and Shu, LS (2009) A Paleoproterozoic orogeny recorded in a long-lived cratonic remnant (Wuyishan terrane), eastern Cathaysia Block, China. Precambrian Research 174, 347–63.CrossRefGoogle Scholar
Zhai, MG (2011) Cratonization and the formation of the North China block. Science China-Earth Science 41(8), 1037–46.Google Scholar
Zhang, SB and Zheng, YF, (2013) Formation and evolution of Precambrian continental lithosphere in South China. Gondwana Research 23, 1243–60.CrossRefGoogle Scholar
Zhao, G (2015) Jiangnan Orogen in South China: developing from divergent double subduction. Gondwana Research 27(3), 1173–80.CrossRefGoogle Scholar
Zhao, GC and Cawood, PA (2012) Precambrian geology of China. Precambrian Research 222–223, 12–54.Google Scholar
Zhao, L, Zhou, XW, Zhai, MG, Santosh, M, Ma, XD, Shan, HX and Cui, XH (2014) Paleoproterozoic tectonic transition from collision to extension in the eastern Cathaysia Block, South China: evidence from geochemistry, zircon U-Pb geochronology and Nd-Hf isotopes of a granite-charnockite suite in southwestern Zhejiang. Lithos 184–187, 259–80.CrossRefGoogle Scholar
Zheng, YF (2008) A perspective view on ultrahigh-pressure metamorphism and continental collision in the Dabie-Sulu orogenic belt. Chinese Science Bulletin 53(20), 3081–104.Google Scholar
Zhu, J, Wang, R, Lu, J, Zhang, H, Zhang, W, Xie, L and Zhang, R (2011) Fractionation, evolution, petrogenesis and mineralization of Laiziling granite pluton, southern Hunan province. Geological Journal of China Universities 17(3), 381–92 (in Chinese with English abstract).Google Scholar
Supplementary material: File

Li et al. supplementary material

Li et al. supplementary material

Download Li et al. supplementary material(File)
File 79.5 KB