Abstract
A whole-rock geochemical and zircon U–Pb and Lu–Hf isotope study of the Dengfeng complex in the Jishan area was performed to constrain the Neoarchean continental crust evolution in the southern margin of the North China Craton (NCC). The Dengfeng complex can be divided into supracrustal assemblage and plutonic intrusion. In the supracrustal assemblage, the detrital zircon of quartz schist from the Guojiayao Formation display oscillatory growth zones and streaky absorption with relatively high Th/U ratios (0.36–2.10), suggesting a magmatic origin. The 207Pb/206Pb ages range from 2963 to 2531 Ma, with a peak age of 2555 Ma, and the εHf(t) values are between + 2.3 and + 12.1. Combined with previous studies, the depositional age of the Guojiayao Formation can be constrained between 2542 and 2522 Ma, indicating that it mainly originated from the Neoarchean accretive basement material of the southern NCC. The Ruzhou gneissic syenogranites yield U–Pb ages from 2515 ± 13 Ma to 2504 ± 20 Ma, show that the plutonic intrusions also formed in the Late Neoarchean. They have high SiO2 (64.03–73.99 wt%) and Na2O + K2O (8.79–14.58 wt%) contents but low MgO (0.19–0.36 wt%) and CaO (0.02–0.27 wt%) contents, and belong to slightly peraluminous I-type granites with shoshonitic affinity. Magmatic zircon grains have positive εHf(t) values (+ 0.2 to + 6.7) with average crustal Hf model ages ranging from 2911 to 2671 Ma (average of 2765 Ma), indicating that the Ruzhou gneissic syenogranites were likely produced by partial melting of the accretive lower crust. The positive εHf(t) values and similarly ancient model ages suggest that a large-scale continental crust growth occurred in the southern margin of NCC at ca. 2.7 Ga. The Dengfeng complex was mainly derived from an arc-related setting associated with subduction in the Late Neoarchean.
Similar content being viewed by others
Change history
07 January 2023
A Correction to this paper has been published: https://doi.org/10.1007/s00531-022-02283-1
References
Arndt N, Davaille A (2013) Episodic earth evolution. Tectonophys 609:661–674. https://doi.org/10.1016/j.tecto.2013.07.002
Bao C, Chen YL, Li DP et al (2015) Evolutionary history of precambrian continental crust in the North China Craton. Geochem J 49:53–62. https://doi.org/10.2343/geochemj.2.0329
Bea F, Arzamastsev A, Montero P et al (2001) Anomalous alkaline rocks of Soustov, Kola: evidence of mantle-derived metasomatic fluids affecting crustal materials. Contrib Mineral Petr 140(5):554–566. https://doi.org/10.1007/s004100000211
Belousova EA, Griffin WL, O’Reilly SY et al (2002) Igneous zircon: trace element composition as an indicator of source rock type. Contrib Mineral Petrol 143:602–622. https://doi.org/10.1007/s00410-002-0364-7
Belousova EA, Kostitsyn YA, Griffin WL et al (2010) The growth of the continental crust: constraints from zircon Hf-isotope data. Lithos 119(3–4):457–466. https://doi.org/10.1016/j.lithos.2010.07.024
Cawood PA, Hawkesworth CJ, Dhuime B (2013) The continental record and the generation of continental crust. Geol Soc Am Bull 125:14–32. https://doi.org/10.1130/B30722.1
Cawthorn RG, Strong DF, Brown PA (1976) Origin of corundum-normative intrusive and extrusive magmas. Nature 259:102–104. https://doi.org/10.1038/259102a0
Chen Q, Sun M, Zhao G et al (2019) Episodic crustal growth and reworking of the Yudongzi Terrane, south China: constraints from the Archean TTGs and potassic granites and Paleoproterozoic amphibolites. Lithos 326–327:1–18. https://doi.org/10.1016/j.lithos.2018.12.005
Condie KC (1981) Archean greenstone belts. Elsevier Scientific Pub. Co, Amsterdam, pp 3–434
Condie KC, Belousova E, Griffin WL et al (2009) Granitoid events in space and time: constraints from igneous and detrital zircon age spectra. Gondwana Res 15:228–242. https://doi.org/10.1016/j.gr.2008.06.001
Deng H, Kusky T, Polat A et al (2016) A 2.5 Ga fore-arc subduction accretion complex in the Dengfeng granite-greenstone belt, southern North China Craton. Precambr Res 275:241–264. https://doi.org/10.1016/j.precamres.2016.01.024
Diwu CR (2010) Continental crust formation and evolution of southern North China Craton: U-Pb dating and Lu-Hf isotope compositions of the Taihua complex and Dengfeng complex. Dissertation, Northwest University. (in Chinese with English abstract). https://doi.org/10.7666/d.y1679578
Diwu CR, Sun Y, Yuan HL et al (2008) U-Pb ages and Hf isotopes for detrital zircons from quartzite in the Paleoproterozoic Songshan Group on the southwestern margin of the North China Craton. Chinese Sci Bull 53(18):2828–2839. https://doi.org/10.1007/s11434-008-0342-1
Diwu CR, Sun Y, Guo AL et al (2011) Crustal growth in the North China Craton at ~2.5 Ga: evidence from in situ zircon U-Pb ages, Hf isotopes and whole-rock geochemistry of the Dengfeng complex. Gondwana Res 20(1):149–170. https://doi.org/10.1016/j.gr.2011.01.011
Diwu CR, Sun Y, Wang Q (2012) The crustal growth and evolution of North China Craton: revealed by Hf isotopes in detrital zircons from modern rivers. Ac Petrol Sin 28(11):3520–3530 (in Chinese with English abstract)
Diwu CR, Sun Y, Zhao Y et al (2014) Early Paleoproterozoic (2.45–2.20 Ga) magmatic activity during the period of global magmatic shutdown: implications for the crustal evolution of the southern North China Craton. Precambr Res 255:627–640. https://doi.org/10.1016/j.precamres.2014.08.001
Diwu CR, Zhang CL, Sun Y (2016) Archean Continental Crust in the Southern North China Craton. Springer, New York, pp 29–44. https://doi.org/10.1007/978-981-10-1064-4_2
Diwu CR, Wang TY, Yan JH (2020) New evidence for Neoarchean (ca. 2.7 Ga) crustal growth in the North China Craton. Precambr Res 350:1–13. https://doi.org/10.1016/j.precamres.2020.105921
Drummond MS, Defant MJ (1990) A model for Trondhjemite–Tonalite–Dacite genesis and crustal growth via slab melting: Archean to modern comparisons. J Geophys Res 95(B13):21503–21521. https://doi.org/10.1029/JB095iB13p21503
Frost CD, McLaughlin JF, Frost BR et al (2017) Hadean origins of Paleoarchean continental crust in the central Wyoming Province. Geol Soc Am Bull 129:259–280. https://doi.org/10.1130/b31555.1
Griffin WL, Pearson NJ, Belousova E et al (2000) The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochim Cosmochim Acta 64(1):133–147. https://doi.org/10.1016/S0016-7037(99)00343-9
Guo AL, Zhou DW (1990) Archean granite-greenstone belts in central Henan Province. Henan Geol 8(2):32–37 (in Chinese)
Han PY, Guo JL, Chen K et al (2017) Widespread Neoarchean (2.7–2.6 Ga) magmatism of the Yangtze craton, South China, as revealed by modern river detrital zircons. Gondwana Res 42:1–12. https://doi.org/10.1016/j.gr.2016.09.006
Hao LR, Yang HT, Yang DH (2020) U-Pb-Hf isotopes of Neoarchean Shuimowan tonalites in southern margin of North China Craton: constrains on petrogenesis. Glob Geol 23(3):180–190. https://doi.org/10.3969/j.issn.1673-9736.2020.03.06
Huang XL, Wilde SA, Zhong JW (2013) Episodic crustal growth in the southern segment of the Trans-North China Orogen across the Archean–Proterozoic boundary. Precamb Res 233:337–357. https://doi.org/10.1016/j.precamres.2013.05.016
Huang B, Kusky TM, Wang L et al (2019) Structural relationships and kinematics of the Neoarchean Dengfeng forearc and accretionary complexes, southern North China craton. Geol Soc Am Bull 121(5–6):966–996. https://doi.org/10.1130/B31938.1
Huang B, Kusky TM, Johnson TE et al (2020) Paired metamorphism in the Neoarchean: a record of accretionary-to-collisional orogenesis in the North China Craton. Earth Planet Sc Lett 543:116355. https://doi.org/10.1016/j.epsl.2020.116355
Iizuka T, Komiya T, Rino S et al (2010) Detrital zircon evidence for Hf isotopic evolution of granitoid crust and continental growth. Geochim Cosmochim Ac 74(8):2450–2472. https://doi.org/10.1016/j.gca.2010.01.023
Irving AJ, Frey FA (1978) Distribution of trace-elements between garnet megacrysts and host volcanic liquids of kimberlitic to rhyolitic composition. Geochim Cosmochim Ac 42:771–787. https://doi.org/10.1016/0016-7037(78)90092-3
Kroner A, Compston W, Guo WZ et al (1988) Age and tectonic setting of Late Archean greenstone-gneiss terrain in Henan Province, China, as revealed by single-grain zircon dating. Geology 16(3):211–215. https://doi.org/10.1130/0091-7613(1988)016%3c0211:AATSOL%3e2.3.CO;2
Kusky TM, Bradley DC, Haeussler PJ et al (1997) Controls on accretion of flysch and mélange belts at convergent margins: evidence from the Chugach Bay thrust and Iceworm mélange, Chugach accretionary wedge. Alaska Tecton 16(6):855–878. https://doi.org/10.1029/97TC02780
Lao ZQ (1999) Wang SY (1999) New advances in the study of the Dengfeng complex in the Songshan region, Henan Province. Reg Geol China 1:9–16. https://doi.org/10.3969/j.issn.1671-2552.1999.01.002(inChinesewithEnglishabstract)
Li JB (2014) Research in tectonic evolution of Neoarchean Dengfeng group in Songshan area. Dissertation, Henan Polytechnic University (in Chinese with English abstract)
Liu DY, Nutman AP, Compston W et al (1992) Remnants of 3800 Ma crust in the Chinese Part of the Sino-Korean craton. Geology 20(4):339–342. https://doi.org/10.1130/0091-7613(1992)020%3c0339:ROMCIT%3e2.3.CO;2
Liu DY, Wilde SA, Wan Y et al (2009) Combined U-Pb, hafnium and oxygen isotope analysis of zircons from meta-igneous rocks in the southern North China Craton reveal multiple events in the Late Mesoarchean—early Neoarchean. Chemic Geol 261(1–2):140–154. https://doi.org/10.1016/j.chemgeo.2008.10.041
Liu CH, Zhao GC, Sun M et al (2012) Detrital zircon U-Pb dating, Hf isotopes and whole-rock geochemistry from the Songshan Group in the Dengfeng Complex: constraints on the tectonic evolution of the Trans-North China Orogen. Precambr Res 192–195(1):1–15. https://doi.org/10.1016/j.precamres.2011.10.006
Lu SN (1994) Judgement on the rationality of a Sm-Nd isochron. Reg Geol China 13(2):148–159 (in Chinese)
Nédélec A, Trindade R, Peschler A et al (2015) Hydrothermally-induced changes in mineralogy and magnetic properties of oxidized A-type granites. Lithos 212–215:145–157. https://doi.org/10.1016/j.lithos.2014.11.007
Rudnick RL, Gao S (2003) Composition of the continental crust. Treatise Geochem. https://doi.org/10.1016/B0-08-043751-6/03016-4
Shi JP, Yang HT, Yang DB et al (2018) Archean crustal growth and reconstruction of the southern margin of North China Craton: constraints from the U-Pb-Hf isotopic compositions of detrital zircon from the Wuzhiling formation at the Dengfeng area. Geotecton Metallog 42(2): 379–391. https://doi.org/10.16539/j.ddgzyckx.2017.02.016(in Chinese with English abstract)
Sun SS, Mcdonough WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geol Soc London 42(1):313–345. https://doi.org/10.1144/GSL.SP.1989.042.01.19
Tang L, Santosh M (2018) Neoarchean granite-greenstone belts and related ore mineralization in the North China Craton: an overview. Geosci Front 9(3):751–768. https://doi.org/10.1016/j.gsf.2017.04.002
Taylor SR, McLennan SM (1995) The geochemical evolution of the continental crust. Rev Geophys 33(2):241–265. https://doi.org/10.1029/95RG00262
Wan YS, Liu DY, Wang SY et al (2009) Early Precambrian crustal evolution in the Dengfeng area, Henan Province (eastern China): constraints from geochemistry and SHRIMP U-Pb zircon dating. Ac Geol Sin 83(7):982–999. https://doi.org/10.3321/j.issn:0001-5717.2009.07.007 (in Chinese with English abstract)
Wan YS, Liu DY, Wang W et al (2011) Provenance of Meso- to Neoproterozoic cover sediments at the Ming Tombs, Beijing, North China Craton: An integrated study of U-Pb dating and Hf isotopic measurement of detrital zircons and whole-rock geochemistry. Gondwana Res 20(1):219–242. https://doi.org/10.1016/j.gr.2011.02.009
Wang K, Liu SW, Wang MJ et al (2017) Geochemistry and zircon U-Pb-Hf isotopes of the late Neoarchean granodiorite-monzogranite-quartz syenite intrusions in the Northern Liaoning Block, North China Craton: petrogenesis and implications for geodynamic processes. Precambr Res 295:151–171. https://doi.org/10.1016/j.precamres.2017.04.021
Whalen JB, Currie KL, Chappell BW (1987) A-type granites: geochemical characteristics, discrimination and petrogenesis. Contrib Mineral Petr 95(4):407–419. https://doi.org/10.1007/BF00402202
Whitney JA, Stormer JC (1985) Mineralogy, petrology, and magmatic conditions from the Fish Canyon Tuff, Central San Juan volcanic field. Colorado J Petrol 26(3):726–762. https://doi.org/10.1093/petrology/26.3.726
Wu FY, Yang YH, Xie LW et al (2006) Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. Chemic Geol 234(1):105–126. https://doi.org/10.1016/j.chemgeo.2006.05.003
Yang DB, Xu WL, Xu YG et al (2012a) U-Pb ages and Hf isotope data from detrital zircons in the Neoproterozoic sandstones of northern Jiangsu and southern Liaoning Provinces, China: implications for the Late Precambrian evolution of the southeastern North China Craton. Precambr Res 216–219(9):162–176. https://doi.org/10.1016/j.precamres.2012.07.002
Yang J, Cawood PA, Du Y et al (2012b) Large igneous Province and magmatic arc sourced Permian–Triassic volcanogenic sediments in China. Sediment Geol 261–262:120–131. https://doi.org/10.1016/j.sedgeo.2012.03.018
Yang DB, Xu WL, Xu YG et al (2013) Provenance of sediments from Mesozoic basins in western Shandong: implications for the evolution of the North China Block. J Asian Earth Sci 76(2):12–29. https://doi.org/10.1016/j.jseaes.2013.07.027
Yang DB, Xu WL, Zhao GC et al (2016) Tectonic implications of Early Cretaceous low–Mg adakitic rocks generated by partial melting of thickened lower continental crust at the southern margin of the central North China Craton. Gondwana Res 38:220–237. https://doi.org/10.1016/j.gr.2015.11.013
Yang DB, Yang HT, Shi JP et al (2017) Sedimentary response to the paleogeographic and tectonic evolution of the southern North China Craton during the late Paleozoic and Mesozoic. Gondwana Res 49:278–295. https://doi.org/10.1016/j.gr.2017.06.009
Yuan HL, Gao S, Liu XM et al (2004) Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma mass spectrometry. Geostand Geoanaly Res 28(3):353–370. https://doi.org/10.1111/j.1751-908X.2004.tb00755.x
Zen EA (1986) Aluminum enrichment in silicate melts by fractional crystallization: some mineralogic and petrographic constraints. J Petrol 27(5):1095–1117. https://doi.org/10.1093/petrology/27.5.1095
Zhai MG, Guo JH, Liu WJ (2005) Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton. J Asian Earth Sci 24(5):547–561. https://doi.org/10.1016/j.jseaes.2004.01.018
Zhang J, Zhang HF, Lu XX (2013) Zircon U-Pb age and Lu–Hf isotope constraints on Precambrian evolution of continental crust in the Songshan area, the south-central North China Craton. Precambr Res 226:1–20. https://doi.org/10.1016/j.precamres.2012.11.015
Zhang HF, Wang JL, Ding WZ et al (2014) Hadean to Neoarchean episodic crustal growth: Detrital zircon records in Paleoproterozoic quartzites from the southern North China Craton. Precambr Res 254:245–257. https://doi.org/10.1016/j.precamres.2014.09.003
Zhang J, Zhang HF, Li L et al (2018) Neoarchean–Paleoproterozoic tectonic evolution of the southern margin of the north China Craton; insights from geochemical and zircon U-Pb-Hf-O isotopic study of metavolcanic rocks in the Dengfeng complex. Precambr Res 318:103–121. https://doi.org/10.1016/j.precamres.2018.10.008
Zhao GC, Zhai MG (2013) Lithotectonic elements of Precambrian basement in the North China Craton: review and tectonic implications. Gondwana Res 23(4):1207–1240. https://doi.org/10.1016/j.gr.2012.08.016
Zhao GC, Cawood PA, Wilde SA et al (2001) High-pressure granulites (retrograded eclogites) from the Hengshan Complex, North China Craton: petrology and tectonic implications. J Petrol 42(6):1141–1170. https://doi.org/10.1093/petrology/42.6.1141
Zhao GC, Sun M, Wilde SA et al (2005) Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited. Precambr Res 136(2):177–202. https://doi.org/10.1016/j.precamres.2004.10.002
Zheng YF, Zhao GC (2020) Two styles of plate tectonics in Earth’s history. Sci Bull 65(4):329–334. https://doi.org/10.1016/j.scib.2018.12.029
Zhou YY, Zhao TP, Wang CY et al (2011) Geochronology and geochemistry of 25 to 24 Ga granitic plutons from the southern margin of the North China Craton: implications for a tectonic transition from arc to post-collisional setting. Gondwana Res 20(1):171–183. https://doi.org/10.1016/j.gr.2011.03.004
Acknowledgements
This work was financially supported by the Natural Science Foundation of China (42072063, 41722204), the Postgraduate Innovation Research Program of Jilin University (101832020CX199) and the basic Scientific Research Foundation of Central Universities of China (Jilin University).
Author information
Authors and Affiliations
Corresponding author
Additional information
The original online version of this article was revised due to missing of affiliation for corresponding author.
Supplementary Information
Below is the link to the electronic supplementary material.
Rights and permissions
Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Hao, L., Yang, D., Mu, M. et al. Neoarchean continental crust evolution of the southern North China Craton: constrains from geochronology and geochemistry of the Dengfeng complex in the Jishan area. Int J Earth Sci (Geol Rundsch) 112, 161–173 (2023). https://doi.org/10.1007/s00531-022-02248-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00531-022-02248-4