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Arc-related peridotite blocks exhumed to the Eastern Block of the North China Craton prior to 2.47 Ga

Published online by Cambridge University Press:  27 July 2021

Mingyue Gong Open the ORCID record for Mingyue Gong [Opens in a new window] ,
Wei Tian Open the ORCID record for Wei Tian [Opens in a new window] ,
Zhuang Li ,
Bin Fu  and
Chunjing Wei
Mingyue Gong
Affiliation:
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing100871, China
Wei Tian*
Affiliation:
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing100871, China
Zhuang Li
Affiliation:
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing102249, China College of Geosciences, China University of Petroleum, Beijing102249, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun130061, China
Bin Fu
Affiliation:
Research School of Earth Sciences, The Australian National University, CanberraACT2601, Australia
Chunjing Wei
Affiliation:
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing100871, China
*
Author for correspondence: Wei Tian, Email: [email protected]
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Abstract

The Songling and Majiayu peridotite blocks occur in the Eastern Block, North China Craton (NCC). Geothermobarometry data show that the Songling peridotites began exhumation from a depth of c. 70 km (c. 23 kbar). During exhumation, the Songling peridotites were intruded by an upper-crust-derived, high-δ18O (up to +7.28‰ in zircon) trondhjemitic dyke at 2.47 Ga and experienced granulite-facies metamorphism. The Songling peridotites have hybrid mantle wedge (HMW) -like high SiO2 (> 45 wt%), high FeOt (c. 10 wt%) content, high modal orthopyroxene abundance (> 35%) and high ϵNd(t) (+18.4 to +21.4), which were generated by the reaction between peridotite and eclogite-derived melts. The clinopyroxenes from the Songling peridotites were in equilibrium with a Nb-, Zr- and Ti-depleted arc-like magma. The Majiayu peridotites are characterized by depletion of Nb, Zr and Hf and are highly enriched in FeOt, Th and light rare earth elements (LREEs), which can be interpreted as an open system reaction between hydrous melts and fore-arc mantle peridotites. These two peridotite blocks are considered to be arc-related mantle peridotites that experienced melt extraction and metasomatism in different styles. They were exhumed to the north margin of the North China Craton during the c. 2.47 Ga arc–continent collision along the Zunhua structural belt.

Keywords

Neoarcheanperidotitetrondhjemitic dykeNorth China Cratonexhumationarc–continent collision
Type
Original Article
Information
Geological Magazine , Volume 158 , Issue 12 , December 2021 , pp. 2115 - 2138
Copyright
© The Author(s), 2021. Published by Cambridge University Press

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References

Ballhaus, C, Berry, RF and Green, DH (1991) High pressure experimental calibration of the olivine–orthopyroxene–spinel oxygen geobarometer: implications for the oxidation state of the upper mantle. Contributions to Mineralogy and Petrology 107, 27–40.CrossRefGoogle Scholar
Bédard, JH (2006) A catalytic delamination-driven model for coupled genesis of Archaean crust and sub-continental lithospheric mantle. Geochimica et Cosmochimica Acta 70, 1188–14.CrossRefGoogle Scholar
Bédard, JH (2018) Stagnant lids and mantle overturns: implications for Archaean tectonics, magmagenesis, crustal growth, mantle evolution, and the start of plate tectonics. Geoscience Frontiers 9, 19–49.CrossRefGoogle Scholar
Bénard, A, Arculus, RJ, Nebel, O, Ionov, DA and Mcalpine, S (2017) Silica-enriched mantle sources of subalkaline picrite-boninite-andesite island arc magmas. Geochimica et Cosmochimica Acta 199, 287–303.CrossRefGoogle Scholar
Bénard, A, Müntener, O, Pilet, S, Arculus, RJ and Nebel, O (2021) Silica-rich spinel harzburgite residues formed by fractional hybridization-melting of the intra-oceanic supra-subduction zone mantle: new evidence from TUBAF seamount peridotites. Geochimica et Cosmochimica Acta 293, 477–506.CrossRefGoogle Scholar
Beyer, EE, Brueckner, HK, Griffin, WL, O’Reilly, SY and Graham, S (2004) Archean mantle fragments in proterozoic crust, western Gneiss Region, Norway. Geology 32, 609–12.CrossRefGoogle Scholar
Bindeman, IN, Eiler, JM, Yogodzinski, GM, Tatsumi, Y, Stern, CR, Grove, TL, Portnyagin, M, Hoernle, K and Danyushevsky, LV (2005) Oxygen isotope evidence for slab melting in modern and ancient subduction zones. Earth and Planetary Science Letters 235, 496.CrossRefGoogle Scholar
Bodinier, J-L, Garrido, CJ, Chanefo, I, Bruguier, O and Gervilla, F (2008) Origin of pyroxenite– peridotite veined mantle by refertilization reactions: evidence from the Ronda Peridotite (Southern Spain). Journal of Petrology 49, 999–1025.CrossRefGoogle Scholar
Brueckner, HK, Van Roermund, H and Perarson, NJ (2004) An Archean (?) to Paleozoic evolution for a garnet peridotite lens with sub-baltic shield affinity within the Seve Nappe complex of Jamtland, Sweden, Central Scandinavian Caledonides. Journal of Petrology 45, 415–37.CrossRefGoogle Scholar
Condie, KC (2016) A planet in transition: the onset of plate tectonics between 3 and 2 Ga? Geoscience Frontiers 9, 51–60.CrossRefGoogle Scholar
Condie, KC and Kröner, A (2008) When did plate tectonics begin? Evidence from the geologic record. In When Did Plate Tectonics begin on Planet Earth? (eds Condie, KC and Pease, V), pp. 281–94. Geological Society of America, Boulder, Special Paper no. 440.CrossRefGoogle Scholar
Cuthbert, SJ and Carswell, DA (1990) Formation and exhumation of medium-temperature eclogites in the Scandinavian Caledonides. In Eclogite Facies Rocks (ed. Carswell, DA), pp. 180–203. New York: Chapman and Hall.CrossRefGoogle Scholar
Cuthbert, SJ, Harvey, MA and Carswell, DA (1983) A tectonic model for the metamorphic evolution of the Basal Gneiss Complex, Western South Norway. Journal of Metamorphic Geology 1, 63–90.CrossRefGoogle Scholar
Deng, H, Kusky, TM, Polat, A, Wang, C, Wang, L, Li, YX and Wang, JP (2016) A 2.5 Ga fore–arc subduction–accretion complex in the Dengfeng Granite-Greenstone Belt, Southern North China Craton. Precambrian Research 275, 241–64.CrossRefGoogle Scholar
Deng, H, Kusky, TM, Polat, A, Wang, L, Wang, JP and Wang, SJ (2013) Geochemistry of Neoarchean mafic volcanic rocks and late mafic dikes in the Zanhuang Complex, Central Orogenic Belt, North China Craton: implications for geodynamic setting. Lithos 175–176, 193–212.CrossRefGoogle Scholar
Duan, ZZ, Wei, CJ and Rehman, HU (2017) Metamorphic evolution and zircon ages of pelitic granulites in eastern Hebei, North China Craton: insights into the regional Archean P–T–t history. Precambrian Research 292, 240–57.CrossRefGoogle Scholar
Eggins, SM, Grun, R, McCulloch, MT, Pike, AWG, Chappell, J, Kinsley, L, Mortimer, G, Shelley, M, Murray-Wallace, CV, Spotle, C and Taylor, L (2005) In situ U-series dating by laser-ablation multi-collector ICPMS: new prospects for Quaternary geochronology. Quaternary Science Reviews 24, 2523–38.CrossRefGoogle Scholar
Eiler, JM (2001) Oxygen isotope variations of basaltic lavas and upper mantle rocks. Reviews in Mineralogy and Geochemistry 43, 319–64.CrossRefGoogle Scholar
Ferry, JM and Watson, EB (2007) New thermodynamic models and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers. Contributions to Mineralogy and Petrology 154, 429–37.CrossRefGoogle Scholar
Fu, B, Bröcker, M, Ireland, T, Holden, P and Kinsley, LPJ (2015) Zircon U–Pb, O, and Hf isotopic constraints on Mesozoic magmatism in the Cyclades, Aegean Sea, Greece. International Journal of Earth Sciences 104, 75–87.CrossRefGoogle Scholar
Gao, S, Rudnick, RL, Xu, WL, Yuan, HL, Liu, YS, Walker, RJ, Puchtel, IS, Liu, XM, Huang, H, Wang, XR and Yang, J (2008) Recycling deep cratonic lithosphere and generation of intraplate magmatism in the North China craton. Earth and Planetary Science Letters 270, 41–53.CrossRefGoogle Scholar
Geng, YS, Liu, FL and Yang, CH (2006) Magmatic event at the end of the Archean in Eastern Hebei province and its geological implication. Acta Geologica Sinica (English Edition) 80, 819–33.Google Scholar
Goldstein, SL, O’Nions, RK and Hamilton, PJ (1984) A Sm–Nd study of atmospheric dusts and particulates from major river systems. Earth Planetary Science Letters 70, 221–36.CrossRefGoogle Scholar
Green, E, Hooland, T and Powell, R (2007) An order–disorder model for omphacitic pyroxenes in the system jadeite-dispside-hedenbergite-acmite, with application to eclogitic rocks. American Mineralogist 92, 1181–89.CrossRefGoogle Scholar
Griffin, WL, Powell, WJ, Pearson, NJ and O’Reilly, SY (2008) Glitter: data reduction software for laser ablation ICP-MS. In Laser Ablation ICP-MS in the Earth Sciences: Current Practices and Outstanding Issues (ed. Sylvester, PJ), pp. 308–11. Vancouver, BC: Mineralogical Association of Canada Short Course Series, Short Course 40.Google Scholar
Hanchar, JM and Miller, CF (1993) Zircon zonation patterns as revealed by cathodoluminescence and back-scattered eletron images: implications for interpretation of complex crustal histories. Chemical Geology 110, 1–13.CrossRefGoogle Scholar
Hauri, EH, Wagner, TP and Grove, TL (1994) Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic melts. Chemical Geology 117, 149–66.CrossRefGoogle Scholar
Herzberg, C (2004) Geodynamic information in peridotite petrology. Journal of Petrology 45, 2507–30.CrossRefGoogle Scholar
Herzberg, C (2011) Identification of source lithology in the Hawaiian and Canary Islands: implications for origins. Journal of Petrology 52, 113–46.CrossRefGoogle Scholar
Herzberg, C and O’Hara, MJ (2002) Plume-associated ultramafic magmas of Phanerozoic age. Journal of Petrology 43, 1857–83.CrossRefGoogle Scholar
Hoskin, P and Black, LP (2000) Metamorphic zircon formation by solid-state recrystallize-tion of protolith igneous zircon. Journal of Metamorphic Geology 18, 423–39.CrossRefGoogle Scholar
Ionov, DA, Chazot, G, Chauvel, C, Merlet, C and Bodinier, J-L (2006) Trace element distribution in peridotite xenoliths from Tok, SE Siberian craton: a record of pervasive, multistage metasomatism in shallow refractory mantle. Geochimica et Cosmochimica Acta 70, 1231–60.CrossRefGoogle Scholar
Ireland, TR and Williams, IS (2003) Considerations in zircon geochronology by SIMS. Reviews in Mineralogy and Geochemistry 53, 215–41.CrossRefGoogle Scholar
Kamenetsky, VS, Crawford, AJ and Meffre, S (2001) Factors controlling chemistry of magmatic spinel: an empirical study of associated olivine, Cr-spinel and melt inclusions from primitive rocks. Journal of Petrology 42, 655–71.CrossRefGoogle Scholar
Kusky, TM and Li, JH (2003) Paleoproterozoic tectonic evolution of the North China craton. Journal of Asian Earth Sciences 22, 383–97.CrossRefGoogle Scholar
Kusky, TM, Li, JH and Tucker, RD (2001) The Archean Dongwanzi Ophiolite Complex, North China Craton: 2.505-billion-year-old oceanic crust and mantle. Science 292, 1142–45.CrossRefGoogle ScholarPubMed
Kusky, TM, Polat, A, Windley, BF, Burke, KC, Dewey, JF, Kidd, WSF, Maruyama, S, Wang, JP, Deng, H, Wang, ZS, Wang, C, Fu, D, Li, XW and Peng, HT (2016) Insights into the tectonic evolution of the North China Craton through comparative tectonic analysis: a record of outward growth of Precambrian continents. Earth Science Reviews 162, 387–432.CrossRefGoogle Scholar
Kusky, TM, Wang, JP, Wang, L, Huang, B, Ning, WB, Fu, D, Peng, HT, Deng, H, Polat, A, Zhang, YT and Shi, GZ (2020) Melanges through time: life cycle of the world’s largest Archean melange compared with Mesozoic and Paleozoic subduction-accretion-collision melanges. Earth Science Reviews 209, 103303.CrossRefGoogle Scholar
Kusky, TM, Wang, L, Dilek, Y, Robinson, P, Peng, SB and Huang, XY (2011) Application of the modern ophiolite concept with special reference to Precambrian ophiolites. Science China-Earth Sciences 54, 315–41.CrossRefGoogle Scholar
Kusky, TM, Windley, BF and Zhai, MG (2007) Tectonic evolution of the North China Block: from orogen to craton to orogen. In Mesozoic Sub-continental Lithospheric Thinning under Eastern Asia (eds Zhai, MG, Windley, BF, Kusky, TM and Meng, QR), pp. 1–34. Geological Society of London, Special Publication no. 280.Google Scholar
Kylander-Clark, ARC, Hacker, BR and Cottle, JM (2013) Laser-ablation split-stream ICP petrochronology. Chemical Geology 345, 99–112.CrossRefGoogle Scholar
Lambart, S, Laporte, D, Provost, A and Schiano, P (2012) Fate of pyroxenite-derived melts in the peridotitic mantle: thermodynamic and experimental constraints. Journal of Petrology 53, 451–76.CrossRefGoogle Scholar
Le Maitre, RW (1982) A Classification of Igneous Rocks and Glossary of Terms. London: Blackwell Scientific Publications.Google Scholar
Leake, BE, Woolley, AR, Arps, CES, Birch, WD, Gilbert, MC, Grice, JD, Hawthorne, FC, Kato, A, Kisch, HJ, Krivovichev, VG, Linthout, K, Laird, J, Mandarino, JA, Maresch, WV, Nickel, EH, Rock, NMS, Schumacher, JC, Smith, DC, Stephenson, NCN, Ungaretti, L, Whittaker, EJW and Guo, YZ (1997) Nomenclature of amphiboles: report of the subcommittee on amphiboles of the international mineralogical association, commission on new minerals and mineral names. American Mineralogist 82, 1019–37.Google Scholar
Li, JH and Kusky, TM (2007) A Late Archean foreland fold and thrust belt in the North China Craton: implications for early collisional tectonics. Gondwana Research 12, 47–66.CrossRefGoogle Scholar
Li, JH, Kusky, TM and Huang, X (2002) Archean podiform chromitites and mantle tectonites in Ophiolitic Mélange, North China Craton: a record of early oceanic mantle processes. GSA Today 12, 4–11.2.0.CO;2>CrossRefGoogle Scholar
Li, SG, Xiao, YL, Liou, DL, Chen, YZ, Ge, NJ, Zhang, ZQ, Sun, SS, Cong, BL, Zhang, RY, Hart, SR and Wang, SS (1993) Collision of the North China and Yangtze blocks and formation of coesite-bearing eclogites – timing and processes. Chemical Geology 109, 89–111.CrossRefGoogle Scholar
Lin, Y, Zhang, CH, Li, CM and Deng, HD (2020) From dextral contraction to sinistral extension of intracontinental transform structures in the Yanshan and northern Taihang Mountain belts during Early Cretaceous: implications to the destruction of the North China Craton. Journal of Asian Earth Sciences 189, 104139.CrossRefGoogle Scholar
Liu, DY, Nutman, AP, Compston, W, Wu, JS and Shen, QH (1992) Remnants of ≥3800 Ma crust in the Chinese part of the Sino-Korean craton. Geology 20, 339–42.2.3.CO;2>CrossRefGoogle Scholar
Liu, F, Guo, JH, Lu, XP and Diwu, CR (2009) Crustal growth at 2.5 Ga in the North China Craton: evidence from whole-rock Nd and zircon Hf isotopes in the Huai’an geneiss terrane. Chinese Science Bulletin 24, 4704–13.Google Scholar
Liu, T, Wei, CJ, Kröner, A, Han, BF and Duan, ZZ (2019) Metamorphic P–T paths for the Archean Caozhuang supracrustal sequence, eastern Hebei Province, North China Craton: implications for a sagduction regime. Precambrian Research 340, 105346.CrossRefGoogle Scholar
Ludwig, KR (2001a) User’s Manual for Isoplot/Ex rev. 2.49: a Geochronological Toolkit for Microsoft Excel. Berkeley Geochronological Center, Special Publication no. 1.Google Scholar
Ludwig, KR (2001b) SQUID 1.02, A User’s Manual. Berkeley Geochronological Center, Special Publication no. 2.Google Scholar
Maury, RC, Defant, MJ and Joron, JL (1992) Metasomatism of the sub-arc mantle inferred from trace elements in Philippine xenoliths. Nature 360, 661–3.CrossRefGoogle Scholar
McInnes, BIA, Gregoire, M, Binns, RA, Herzig, PM and Hannington, MD (2001) Hydrous metasomatism of oceanic sub-arc mantle, Lihir, Papua New Guinea: petrology and geochemistry of fluid-metasomatised mantle wedge xenoliths. Earth and Planetary Science Letters 188, 169–83.CrossRefGoogle Scholar
Medaris, LG and Carswell, DA (1990) Petrogenesis of Mg-Cr garnet peridotites in European metamorphic belts. In Eclogite Facies Rocks (ed. Carswell, DA), pp. 260–90. New York: Chapman & Hall.CrossRefGoogle Scholar
Melekhova, E, Blundy, J, Robertson, R and Humphreys, MCS (2015) Experimental evidence for polybaric differentiation of primitive arc basalt beneath St. Vincent, Lesser Antilles. Journal of Petrology 56, 161–92.CrossRefGoogle Scholar
Ning, WB, Kusky, TM, Wang, JP, Wang, L, Deng, H, Polat, A, Huang, B, Peng, HT and Feng, P (2020) From subduction initiation to arc–polarity reversal: life cycle of an Archean subduction zone from the Zunhua ophiolitic mélange, North China Craton. Precambrian Research 350, 105868.CrossRefGoogle Scholar
Niu, YL (2004) Bulk-rock major and trace element compositions of abyssal peridotites: implications for mantle melting, melt extraction and post-melting processes beneath mid-ocean ridges. Journal of Petrology 45, 2423–458.CrossRefGoogle Scholar
Nutman, AP, Wan, YS, Du, LL, Friend, CRL, Dong, CY, Xie, HQ, Wang, W, Sun, HY and Liu, DY (2011) Multistage late Neoarchaean crustal evolution of the North China Craton, eastern Hebei. Precambrian Research 189, 43–65.CrossRefGoogle Scholar
O’Neill, H St C (1981) The transition between spinel lherzolite and garnet lherzolite, and its use as a geobarometer. Contributions to Mineralogy and Petrology 77, 185–94.CrossRefGoogle Scholar
Paterson, BA, Stephens, WE, Rogers, G, Williams, IS, Hinton, RW and Herd, DA (1992) The nature of zircon inheritance in two granite plutons. Transactions of the Royal Society of Edinburgh: Earth Science 83, 459–71.CrossRefGoogle Scholar
Paton, C, Hellstrom, J, Paul, B, Woodhead, J and Hergt, J (2011) Iolite: freeware for the visualisation and processing of mass spectrometric data. Journal of Analytical Atomic Spectrometry 26, 2508–18.CrossRefGoogle Scholar
Paton, C, Woodhead, J, Hellstrom, J, Hergt, J, Greig, A and Maas, R (2010) Improved laser ablation U–Pb zircon geochronology through robust downhole fractionation correction. Geochemistry, Geophysics, Geosystems 11, 1–36.CrossRefGoogle Scholar
Paulick, H, Bach, W, Godard, M, De Hoog, JCM, Suhr, G and Harvey, J (2006) Geochemistry of abyssal peridotites (Mid-Atlantic Ridge, 15°20’N, ODP Leg 209): implications for fluid/rock interaction in slow spreading environments. Chemical Geology 234, 179–210.CrossRefGoogle Scholar
Pearson, DG, Canil, D and Shirey, SB (2014) Mantle samples included in volcanic rocks: xenoliths and diamonds. In Treatise on Geochemistry (2nd edn) (ed. Carlson, RW), pp. 169–253. Netherlands: Elsevier.CrossRefGoogle Scholar
Podvin, P (1988) Ni-Mg partitioning between synthetic olivines and orthopyroxenes: application to geothermometry. American Mineralogist 73, 274–80.Google Scholar
Polat, A, Fryera, BJ, Samsona, IM, Weisener, C, Appel, PWU, Frei, R and Windley, BF (2012) Geochemistry of ultramafic rocks and hornblendite veins in the Fiskenæsset layered anorthosite complex, SW Greenland: evidence for hydrous upper mantle in the Archean. Precambrian Research 214–215, 24–153.Google Scholar
Polat, A, Herzberg, C, Münker, C, Rodgers, R, Kusky, TM, Li, JH, Fryer, BJ and Delancy, J (2006) Geochemical and petrological evidence for a suprasubduction zone origin of Neoarchean (ca. 2.5 Ga) peridotites, central orogenic belt, North China craton. GSA Bulletin 118, 771–84.CrossRefGoogle Scholar
Powell, R and Holland, T (1998) An internally consistent thermodynamic data set for phases of petrological interest. Journal of Metamorphic Geology 16, 309–43.Google Scholar
Powell, R and Holland, T (1999) Relating formulations of the thermodynamics of mineral solid solutions: activity modeling of pyroxenes, amphiboles, and micas. American Mineralogist 84, 1–14.CrossRefGoogle Scholar
Putirka, K (2016) Amphibole thermometers and barometers for igneous systems and implications for eruption mechanisms of felsic magmas at arc volcanoes. American Mineralogist 101, 841–58.CrossRefGoogle Scholar
Qi, HL, Hao, XH, Zhang, XD and Nie, WD (1999) The geological features of granite greenstone belts in Qinglong river, Jidong. Precambrian Research 22, 1–17 (in Chinese with English abstract).Google Scholar
Salters, VJM and White, WM (1998) Hf isotope constraints on mantle evolution. Chemical Geology 145, 447–60.CrossRefGoogle Scholar
Sawyer, EW (2008) Working with migmatites: nomenclature for the constituent parts. In Working with Migmatites (eds Sawyer, EW & Brown, M). Short Course, 38. Mineral Association of Canada, Québec, 1–28.Google Scholar
Schmidt, MW (1992) Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al-in-hornblende barometer. Contributions to Mineralogy and Petrology 110, 304–10.CrossRefGoogle Scholar
Shirey, SB and Walker, RJ (1998) The Re-Os isotope system in cosmochemistry and high-temperature geochemistry. Annual Review of Earth & Planetary Sciences 26, 423–500.CrossRefGoogle Scholar
Slama, J, Kosler, J, Condon, DJ, Crowley, JL, Gerdes, A, Hanchar, JM, Horstwood, MSA, Morris, GA, Nasdala, L, Norberg, N, Schaltegger, U, Schoene, B, Tubrett, MN and Whitehouse, MJ (2008) Plesovice zircon: a new natural reference material for U–Pb and Hf isotopic microanalysis. Chemical Geology 249, 1–35.CrossRefGoogle Scholar
Stern, RJ (2008) Modern-style plate tectonics began in Neoproterozoic time: an alternative interpretation of Earth’s tectonic history. Geological Society of America Special Papers 440, 265–80.Google 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.Google Scholar
Thompson, RN and Gibson, SA (2000) Transient high temperatures in mantle plume heads inferred from magnesian olivines in Phanerozoic picrites. Nature 407, 502–6.CrossRefGoogle ScholarPubMed
Tian, W, Campbell, IH, Allen, CM, Guan, P, Pan, WQ, Chen, MM, Yu, HJ and Zhu, WP (2010) The Tarim picrite–basalt–rhyolite suite, a Permian flood basalt from Northwest China with contrasting rhyolites produced by fractional crystallization and anatexis. Contributions to Mineralogy and Petrology 160, 407–25.CrossRefGoogle Scholar
Tian, W, Wang, SY, Liu, FL, Chu, ZY, Wang, B, Chen, MM and Prichard, J (2017) Archean–Paleoproterozoic lithospheric mantle at the northern margin of the North China Craton represented by tectonically exhumed peridotites. Acta Petrologica Sinica (English Edition) 91, 105–21.Google Scholar
Valley, JW, Lackey, JS, Cavosie, AJ, Clechenko, CC, Spicuzza, MJ, Basei, MAS, Bindeman, IN, Ferreira, VP, Sial, AN and King, EM (2005) 4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon. Contributions to Mineralogy and Petrology 150, 561–80.CrossRefGoogle Scholar
van Roermund, H (2009) Mantle-wedge garnet peridotites from the northernmost ultra-high pressure domain of the Western Gneiss Region, SW Norway. European Journal of Mineralogy 21, 1085–96.CrossRefGoogle Scholar
Vavra, G (1990) On the kinematics of zircon growth and its petrogenetic significance: a cathodoluminescence study. Contributions to Mineralogy and Petrology 106, 90–99.CrossRefGoogle Scholar
Vavra, G, Gebauer, D, Schmid, R and Compston, W (1996) Multiple zircon growth and recrystallisation during polyphase Late Carboniferous to Triassic metamorphism in granulites of the Ivrea Zone (Southern Alps): an ion microprobe (SHRIMP) study. Contributions to Mineralogy and Petrology 122, 337–58.CrossRefGoogle Scholar
Vernières, J, Godard, M and Bodinier, J-L (1997) A plate model for the simulation of trace element fractionation during partial melting and magma transport in the Earth’s upper mantle. Journal of Geophysical Research - Solid Earth 102, 24771–84.CrossRefGoogle Scholar
Walter, MJ (1998) Melting of garnet peridotite and the origin of komatiite and depleted lithosphere. Journal of Petrology 39, 29–60.CrossRefGoogle Scholar
Walter, MJ (2003) Melt extraction and compositional variability in mantle lithosphere. Treatise on Geochemistry, second edition (ed. RW Carlson). Elsevier, 363–394.CrossRefGoogle Scholar
Wan, YS, Liu, DY, Song, B, Wu, JS, Yang, CH, Zhang, ZQ and Geng, YS (2005) Geochemical and Nd isotopic compositions of 3.8 Ga meta-quartz dioritic and trondhjemitic rocks from the Anshan area and their geological significance. Journal of Asian Earth Sciences 24, 563–75.CrossRefGoogle Scholar
Wang, C, Song, S, Wei, C, Su, L and Dong, J (2019a) Palaeoarchaean deep mantle heterogeneity recorded by enriched plume remnants. Nature Geoscience 12, 672–78.CrossRefGoogle Scholar
Wang, CG, Lo Casciob, M, Yan, L and Xua, WL (2020) An experimental study of peridotite dissolution in eclogite-derived melts: implications for styles of melt-rock interaction in lithospheric mantle beneath the North China Craton. Geochimica et Cosmochimica Acta 278, 157–76.CrossRefGoogle Scholar
Wang, JP, Kusky, TM, Polat, A, Wang, L, Deng, H and Wang, SJ (2013) A late Archean tectonic mélange in the Central Orogenic Belt, North China Craton. Tectonophysics 608, 929–46.CrossRefGoogle Scholar
Wang, JP, Li, XW, Ning, WB, Kusky, TM, Wang, L, Polat, A and Deng, H (2019b) Geology of a Neoarchean suture: evidence from the Zunhua ophiolitic mélange of the Eastern Hebei Province, North China Craton. Geological Society of America Bulletin 191, 1943–64.CrossRefGoogle Scholar
Wang, Y, Zhou, LY, Liu, SF, Li, JY and Yang, TN (2018) Post-cratonization deformation processes and tectonic evolution of the North China Craton. Earth Science Review 177, 320–65.CrossRefGoogle Scholar
Watson, EB and Liang, Y (1995) A simple model for sector zoning in slowly grown crystals: implications for growth rate and lattice diffusion, with emphasis on accessory minerals in crustal rocks. American Mineralogist 80, 1179–87.CrossRefGoogle Scholar
Wei, CJ and Duan, ZZ (2019) Phase relations in metabasic rocks: constraints from the results of experiments, phase modelling and ACF analysis. In HP-UHP Metamorphism and Tectonic Evolution of Orogenic Belts (eds Zhang, LF, Zhang, ZM, Schertl, HP and Wei, CJ), pp. 25–45. Geological Society of London, Special Publication no. 474.Google Scholar
White, RW, Powell, R and Holland, T (2007) Progress relating to calculation of partial melting equilibria for metapelites. Journal of Metamorphic Geology 25, 511–27.CrossRefGoogle Scholar
Wiedenbeck, M, Alle, P, Corfu, F, Griffin, WL, Meier, M, Oberli, F, Von Quadt, A, Roddick, JC and Spiegel, W (1995) Three natural zircon standards for U–Th–Pb, Lu–Hf, trace element and REE analyses. Geostandards Newsletter 19, 1–23.CrossRefGoogle Scholar
Witt-Eickschen, G and Kramm, U (1997) Mantle upwelling and metasomatism beneath Central Europe: geochemical and isotopic constraints from mantle xenoliths from the Rhön (Germany). Journal of Petrology 4, 479–93.CrossRefGoogle Scholar
Witt-Eickschen, G and Seck, HA (1991) Solubility of Ca and Al in orthopyroxene from spinel peridotite: an improved version of an empirical geothermometer. Contributions to Mineralogy and Petrology 106, 431–39.CrossRefGoogle Scholar
Wood, BJ and Blundy, JD (1997) A predictive model for rare earth element partitioning between clinopyroxene and anhydrous silicate melt. Contributions to Mineralogy and Petrology 129, 166–81.CrossRefGoogle Scholar
Woodhead, JD and Hergt, JM (2005) A preliminary appraisal of seven natural zircon reference materials for in situ Hf isotope determination. Geostandards and Geoanalytical Research 29, 183–95.CrossRefGoogle Scholar
Woodhead, JD, Hergt, J, Shelley, M, Eggins, S and Kemp, R (2004) Zircon Hf-isotope analysis with an excimer laser, depth profiling, ablation of complex geometries, and concomitant age estimation. Chemical Geology 209, 121–35.CrossRefGoogle Scholar
Wu, JS, Geng, YS, Shen, QH, Wan, YS, Liu, DY and Song, B (1998) Archean Geology Characteristics and Tectonic Evolution of Sino-Korea Paleo-continent. Beijing: Geological Publishing House, 212 p. (in Chinese).Google Scholar
Xiao, WJ, Windley, BF, Hao, J and Zhai, MG (2003) Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: termination of the central Asian orogenic belt. Tectonics 22, 1069.CrossRefGoogle Scholar
Xiong, Q, Griffin, WL, Zheng, JP, O’Reilly, SY and Pearson, NJ (2015) Episodic refertilization and metasomatism of Archean mantle: evidence from an orogenic peridotite in North Qaidam (NE Tibet, China). Contributions to Mineralogy and Petrology 169, 31.CrossRefGoogle Scholar
Yang, C and Wei, CJ (2017) Ultrahigh temperature (UHT) mafic granulites in the East Hebei, North China Craton: constraints from a comparison between temperatures derived from REE-based thermometers and major element-based thermometers. Gondwana Research 46, 156–69.CrossRefGoogle Scholar
Yang, QY, Santosh, M and Tsunogae, T (2016) High–grade metamorphism during Archean-Paleoproterozoic transition associated with microblock amalgamation in the North China Craton: mineral phase equilibria and zircon geochronology. Lithos 263, 101–21.CrossRefGoogle Scholar
Zhai, MG and Santosh, M (2011) The early Precambrian odyssey of North China Craton: a synoptic overview. Gondwana Research 20, 6–25.CrossRefGoogle Scholar
Zhai, MG and Windley, BF (1990) The Archaean and early Proterozoic banded iron formations of North China: their characteristics, geotectonic relations, chemistry and implications for crustal growth. Precambrian Research 48, 267–86.CrossRefGoogle Scholar
Zhang, C, Van Roermund, H and Zhang, LF (2015) Orogenic garnet peridotites: tools to reconstruct paleo-geodynamic settings of fossil continental collision zones. Acta Geologica Sinica 89, 110.CrossRefGoogle Scholar
Zhang, LC, Zhai, MG, Zhang, XJ, Xiang, P, Dai, YP, Wang, CL and Pirajno, F (2012) Formation age and tectonic setting of the Shirengou Neoarchean banded iron deposit in eastern Hebei Province: constraints from geochemistry and SIMS zircon U–Pb dating. Precambrian Research 222–223, 325–38.CrossRefGoogle Scholar
Zhang, SW, Wei, CJ and Duan, ZZ (2017) Petrogenetic simulation of the Archean trondhjemite from eastern Hebei, China. Science China: Earth Sciences 6, 958–71.CrossRefGoogle Scholar
Zhao, GC, Cawood, PA, Li, SZ, Wilde, SA, Sun, M, Zhang, J, He, YH and Yin, CQ (2012) Amalgamation of the North China Craton: key issues and discussion. Precambrian Research 222–223, 55–76.CrossRefGoogle Scholar
Zhao, GC, Sun, M, Wilde, SA and Li, SZ (2005) Late Archean to Paleoproterozoic evolution of the North China craton: key issues revisited. Precambrian Research 136, 177–202.CrossRefGoogle Scholar
Zhao, GC, Wilde, SA, Cawood, PA and Lu, LZ (1998) Thermal evolution of Archean basement rocks from the eastern part of the North China Craton and its bearing on tectonic setting. International Geology Review 40, 706–21.CrossRefGoogle Scholar
Zhao, GC, Wilde, SA, Cawood, PA and Sun, M (2001) Archean blocks and their boundaries in the North China Craton: lithological, geochemical, structural and P–T path constraints and tectonic evolution. Precambrian Research 107, 45–73.CrossRefGoogle Scholar
Zhao, GC, Wilde, SA, Li, S, Sun, M, Grant, ML and Li, X (2007) U–Pb zircon age constraints on the Dongwanzi ultramafic–mafic body, North China, confirm it is not an Archean ophiolite. Earth and Planetary Science Letters 255, 85–93.CrossRefGoogle Scholar
Zhao, GC and Zhai, MG (2013) Lithotectonic elements of Precambrian basement in the North China Craton: review and tectonic implications. Gondwana Research 23, 1207–40.CrossRefGoogle Scholar
Zheng, JP, Griffin, WL, O’Reilly, SY, Lu, FX, Wang, CY, Zhang, M, Wang, FZ and Li, HM (2004) 3.6 Ga lower crust in central China: new evidence on the assembly of the North China craton. Geology 32, 229.CrossRefGoogle Scholar
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