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Variation of oxygen fugacity during magmatic evolution: in-situ geochemistry of mafic dikes from Jiaodong, southeastern North China Craton

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Abstract

Mafic lava is generally used to study the oxygen fugacity of lithospheric mantle. However, some studies confirmed that the high oxygen fugacity of mafic lava from lithospheric mantle may be result of auto-oxidation during the late magma evolution. Whether mafic lava reflects the oxygen fugacity of source area remains controversial. The major and trace element compositions of biotite, amphibole, and plagioclase as well as the Sr isotopes of plagioclase were in-situ examined aim to evaluate the variation in oxygen fugacity of mafic magma during transportation from depth to current location. Mineralogical characteristics show that the dikes originate from an enriched lithospheric mantle source and experienced very little or no crustal contamination during the magma transfer process. Clinopyroxene, plagioclase, Al-rich amphibole, biotite, and Mg-rich amphibole crystallized successively as the depth of magma reduced from 75.9 to 0.8 km. Fayalite-magnetite-quartz (△FMQ) and Ni-NiO (△NNO) are used as reference oxygen fugacity buffers in this study. The average oxygen fugacity of mafic magma gradually increases from △NNO-1.50 (lithospheric mantle source) to △NNO + 2.74 (near the surface) during magma evolution. Calculation results from clinopyroxene, amphibole and biotite show that the oxygen fugacity of magma increases during fractionation of clinopyroxene, plagioclase, amphibole, and biotite. However, the above fractionation cannot generate such a wide variation in oxygen fugacity. Moreover, it is not caused by degassing in terms of the low carbonate mineral content and increasing S6+/Stot ratios during fractionation. Previous studies have shown a rapid cooling and a high H2O content of the Jiaodong mafic magma. Combine with the garnet-spinel transition zone of mantle lithosphere and magnetite observed in petrography, we tend to propose that the variation in oxygen fugacity of mafic magma were caused by magnetite-spinel fractional crystallization at depth. Low-pressure metamorphic amphibole and the country rocks of Late Mesozoic monzodiorite, which has a much higher oxygen fugacity than the stable range of magnetite-spinel, indicated that the secondary alteration in last stage of magma evolution may cause additional variation in oxygen fugacity. In that case, mafic lava cannot be used to determine the oxygen fugacity of source rock.

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References

  • Abdel-Rahman AFM (1994) Nature of biotites from alkaline, calc-alkaline, and peraluminous magmas. J Petrol 35(2):525–541

    Article  Google Scholar 

  • Alia RAM, Iain KP, Ayman EM, Mokhles KA, Bottros RB, Mohamed GS (2020) Petrology and geochemistry of ophiolitic ultramafc rocks and chromitites across the Eastern Desert of Egypt: insights into the composition and nature of a Neoproterozoic mantle and implication for the evolution of SSZ system. Precambrian Res 337:105565

    Article  Google Scholar 

  • Andersen DJ, Lindsley DH (1988) Internally consistent solution models for Fe–Mg–Mn–Ti oxides: Fe–Ti oxides. Am Mineral 73:714–726

  • Anderson JL, Smith DR (1995) The effects of temperature and f02 on the Al-in-hornblende barometer. Am Mineral 80(5):549–559

    Article  Google Scholar 

  • Anderson JL, Barth AP, Wooden JL, Mazdab F (2008) Thermometers and thermobarometers in granitic systems. In: Putirka KD, Tepley FJ III (eds) Minerals, inclusions and volcanic processes. Rev Mineral Geochem, vol 69. Mineral Soc Am, Chantilly, pp 121–142

  • Artemieva IM, Mooney WD (2001) Thermal thickness and evolution of Precambrian lithosphere: a global study. J Geophys Res 106(B8):16387–16414

    Article  Google Scholar 

  • Aulbach S, Woodland AB, Stern RA, Vasilyev P, Heaman LM, Viljoen KS (2019) Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust. Sci Rep 9(1):1–11

    Article  Google Scholar 

  • Aysal N (2015) Mineral chemistry, crystallization conditions and geodynamic implications of the Oligo-Miocene granitoids in the Biga Peninsula, Northwest Turkey. J Asian Earth Sci 105:8–84

  • Ballhaus C (1993) Oxidation states of the lithospheric and asthenospheric upper mantle. Contrib Mineral Petrol 14:331–348

    Article  Google Scholar 

  • Birner SK, Jessica MW, Elizabeth C, Fred AD (2016) Hydrothermal alteration of seafloor peridotites does not influence oxygen fugacity recorded by spinel oxybarometry. Geology 44(7):535–538

    Article  Google Scholar 

  • Brouncea M, Stolpera E, Eiler J (2017) Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation. P Natl Acad Sci USA 114(34):8997–9002

  • Cao YH, Wang CY, Wei B (2019) Magma oxygen fugacity of Permian to Triassic Ni-Cu sulfde-bearing mafc-ultramafc intrusions in the central Asian orogenic belt, North China. J Asian Earth Sci 173:250–262

  • Catanzaro EJ, Murphy TJ, Garner EL, Shields WR (1969) Absolute isotopic abundance ratio and atomic weight of terrestrial rubidium. Journal of research of the National Bureau of Standards. Section A, Physics and chemistry 73:511–516

  • Chen JF, Xie Z, Li HM, Zhang XD, Zhou TX, Park YS, Ahn KS, Chen DG, Zhang X (2003) U–Pb zircon ages for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrane, China. Geochem J 37:35–46

    Article  Google Scholar 

  • Cox SF (2016) Injection-driven swarm seismicity and permeability enhancement: implications for the dynamics of hydrothermal ore systems in high fluid-flux, over-pressured faulting regimes. Econ Geol 111:559–587

    Article  Google Scholar 

  • Dare SAS, Pearce JA, McDonald I, Styles MT (2009) Tectonic discrimination of peridotites using fO2-Cr# and Ga-Ti-FeIII systematics in chrome–spinel. Chem Geol 261:199–216

    Article  Google Scholar 

  • Drake MJ, Weill DF (1975) Partitioning of Sr, Ba, Ca, Y, Eu2+, Eu3+, and other REE between plagioclase feldspar and magmatic liquid: an experimental study. Geochim Cosmochim Acta 39:689–712

  • Deng J, Wang Q (2016) Gold mineralization in China: metallogenic provinces, deposit types and tectonic framework. Gondwana Res 36:219–274

  • Deng J, Wang C, Bagas L, Carranza EJM, Lu Y (2015) Cretaceous–cenozoic tectonic history of the Jiaojia Fault and gold mineralization in the Jiaodong Peninsula, China: constraints from zircon U–Pb, illite K–Ar, and apatite fission track thermochronometry. Miner Depos 50(8):987–1006

  • Deng J, Liu XF, Wang QF, Dilek Y, Liang YY (2017) Isotopic characterization and petrogenetic modeling of early cretaceous mafic diking-lithospheric extension in the North China Craton, eastern Asia. Geol Soc Am Bull 129(11–12):1379–1407

  • Deng J, Wang CM, Bagas L, Santosh M, Yao EY (2018) Crustal architecture and metallogenesis in the south-eastern North China Craton. Earth-Sci Rev 182:251–272

  • Deng J, Qiu KF, Wang QF, Goldfarb R, Yang LQ, Zi JW, Geng JZ, Ma Y (2020) In situ dating of hydrothermal monazite and implications for the geodynamic controls on ore formation in the Jiaodong gold province, eastern China. Econ Geol 115(3):671–685

    Article  Google Scholar 

  • Dilek Y, Sandvol E (2009) Seismic structure, crustal architecture and tectonic evolution of the Anatolian-African plate boundary and the Cenozoic orogenic belts in the eastern Mediterranean region. In: Murphy JB, Keppie JD, Hynes AJ (eds.). Ancient Orogens and modern analogues. Geol Soc Lond, Spec Publ 327(1):127–160

    Article  Google Scholar 

  • Elburg M, Vroon P, Wagt B, Tchalikian A (2005) Sr and Pb isotopic composition of five USGS glasses (BHVO-2G, BIR-1G, BCR-2G, TB-1G, NKT-1G). Chem Geol 223(4):196–207

    Article  Google Scholar 

  • Ersoy EY, Helvac C, Palmer MR (2010) Mantle source characteristics and melting models for the early-middle Miocene mafic volcanism in Western Anatolia: implications for enrichment processes of mantle lithosphere and origin of K-rich volcanism in post-collisional settings. J Volcanol Geoth Res 198:112–128

    Article  Google Scholar 

  • Evans KA (2012) The redox budget of subduction zones. Earth-Sci Rev 113:11–32

    Article  Google Scholar 

  • Evans KA, Reddy SM, Tomkins AG, Crossley RJ, Frost BR (2017) Effects of geodynamic setting on the redox state of fluids released by subducted mantle lithosphere. Lithos 278:26–42

    Article  Google Scholar 

  • Foden J, Paolo AS, Christine MW (2015) Fe isotopes and the contrasting petrogenesis of A-, I- and S-type granite. Lithos 212–215:32–44

    Article  Google Scholar 

  • Gaillard F, Scaillet B, Pichavant M, Beny JL (2001) The effect of water, f02 on the ferric–ferrous ratio of silicic melts. Chem Geol 174:255–273

  • Goss SC, Wilde SA, Wu FY, Yang JH (2010) The age, isotopic signature and significance of the youngest Mesozoic granitoids in the Jiaodong terrane, Shandong province, North China Craton. Lithos 120(3–4):309–326

  • Henry DJ, Guidotti CV, Thomson JA (2005) The Ti-saturation surface for low-to-medium pressure metapelitic biotites: implications for geothermometry and Ti-substitution mechanisms. Am Mineral 90(2–3):316–328

    Article  Google Scholar 

  • Hofmann AW, Jochum KP, Seufert M, White WM (1986) Nb and Pb in oceanic basalts: new constraints on mantle evolution. Earth Planet Sci Lett 79:33–45

    Article  Google Scholar 

  • Holloway JR (2004) Redox reactions in seafloor basalts: possible insights into silicic hydrothermal systems. Chem Geol 210:225–230

    Article  Google Scholar 

  • Hollister LS, Grissom GC, Peters EK, Stowell HH, Sisson VB (1987) Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons. Am Mineral 72(3–4):231–239

    Google Scholar 

  • Hou ML, Jiang YH, Jiang SY, Ling HF, Zhao KD (2007) Contrasting origins of late Mesozoic adakitic granitoids from the northwestern Jiaodong Peninsula, East China: implications for crustal thickening to delamination. Geol Mag 144:619–631

  • Huang XL, He PL, Wang X, Zhong JW, Xu YG (2016) Lateral variation in oxygen fugacity and halogen contents in early cretaceous magmas in Jiaodong area, East China: implication for triggers of the destruction of the North China Craton. Lithos 248:478–492

  • Jiang YH, Jiang SY, Ling HF, Ni P (2010) Petrogenesis and tectonic implications of late Jurassic shoshonitic lamprophyre dikes from the Liaodong Peninsula, NE China. Mineral Petrol 100(3–4):127–151

  • Jochum KP, Weis U, Stoll B, Kuzmin D, Yang QC, Raczek I, Jacob DE, Stracke A, Birbaum K, Frick DA, Günther D, Enzweiler J (2011) Determination of reference values for NIST SRM 610–617 glasses following ISO guidelines. Geostand Geoanal Res 35(4):397–429

    Article  Google Scholar 

  • Johnson MC, Rutherford MJ (1989) Experimental calibration of the aluminium-in- hornblende geobarometer with application to Long Valley caldera (California) volcanic rocks. J Geol 17(9):837–841

    Article  Google Scholar 

  • Kilgore ML, Anne HP, Alan DB, William ML (2018) Water and oxygen fugacity in the lithospheric mantle wedge beneath the northern Canadian cordillera (Alligator Lake). Geochem Geophys Geosyst 19:3844–3869

    Article  Google Scholar 

  • Kostrovitsky SI, Yakovleva DA, Soltysd A, Ivanove AS, Matsyukf SS, Robles-Cruz SE (2020) A genetic relationship between magnesian ilmenite and kimberlites of the Yakutian diamond fields. Ore Geol Rev 120:103419

    Article  Google Scholar 

  • Kudo AM, Weill DF (1970) An igneous plagioclase thermometer. Contrib Mineral Petrol 25(1):52–65

    Article  Google Scholar 

  • Kumar S, Pathak M (2010) Mineralogy and geochemistry of biotites from Proterozoic granitoids of western Arunachal Himalaya: evidence of bimodal granitogeny and tectonic affinity. J Geol Soc India 75(5):715–730

    Article  Google Scholar 

  • 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, 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-Sci Rev 162:387–432

  • Lee CTA, Leeman WP, Canil D, Li XA (2005) Similar V/Sc systematics in MORB and arc basalts: implications for the oxygen fugacities of their mantle source regions. J Petrol 46:2313–2336

    Article  Google Scholar 

  • Lee CTA, Erdman M, Yang WB, Ingramd L, Chin EJ, DePaolo DJ (2018) Sulfur isotopic compositions of deep arc cumulates. Earth Planet Sci Lett 500:76–85

    Article  Google Scholar 

  • Liang YY, Deng J, Liu XF, Wang QF, Qin C, Li Y, Yang Y, Zhou M, Jiang JY (2018) Major and trace element, and Sr isotope compositions of clinopyroxene phenocrysts in mafic dykes on Jiaodong peninsula, southeastern North China Craton: insights into magma mixing and source metasomatism. Lithos 302-303:480–495

  • Liang YY, Deng J, Liu XF, Wang QF, Ma Y, Gao TX, Zhao, LH (2019) Water contents of early cretaceous mafic dikes in the Jiaodong Peninsula, Eastern North China craton: insights into an enriched lithospheric mantle source metasomatized by paleo–pacific plate subduction–related fluids. J Geol 127(3):343–362

  • Liang YY, Deng J, Liu XF, Wang QF, Ma Y, Gao TX, Zhao EQ, Zhou ZH (2020) Geochronology and geochemistry of the palaeoproterozoic mafc dikes in the Jiaobei terrane: implications for tectonic evolution of the Jiao-Liao-Ji Belt, eastern North China Craton. Int Geol Rev https://doi.org/10.1080/00206814.2020.1746932

  • Liu S, Hu RZ, Gao S, Feng CX, Yu BB, Feng GY, Qi YQ, Wang T, Coulson IM (2009) Petrogenesis of late Mesozoic mafic dykes in the Jiaodong Peninsula, eastern North China Craton and implications for the foundering of lower crust. Lithos 113(3–4):621–639

  • Liu XF, Deng J, Liang YY, Wang QF, Pan RG, Qing C, Yang Y (2018) Petrogenesis of early cretaceous intermediate-felsic dikes in the Jiaodong Peninsula, south-eastern North China Craton: constraints from geochronology, geochemistry and Sr-Nd-Pb-Hf isotopes. Gondwana Res 60:69–93

  • Liu YS, Hu ZC, Gao S, Günther D, Xu J, Gao CG, Chen HH (2008) In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chem Geol 257(1–2):34–43

    Article  Google Scholar 

  • Ma L, Jiang SY, Hofmann AW, Dai BZ, Hou ML, Zhao KD, Chen LH, Li WJ, Jiang HY (2014) Lithospheric and asthenospheric sources of lamprophyres in the Jiaodong Peninsula: a consequence of rapid lithospheric thinning beneath the North China Craton? Geochim Cosmochim Acta 124:250–271

  • Ma L, Jiang SY, Hofman AW, Xu YG, Dai BZ, Hou ML (2016) Rapid lithospheric thinning of the North China Craton: new evidence from cretaceous mafic dikes in the Jiaodong Peninsula. Chem Geol 432:1–15

  • Ma Y, Liu XF, Liang YY, Yang Y (2019) Microregional Geochemical Characteristics of Rock-forming Minerals in Early Cretaceous Intermediate-felsic Dikes in Jiaodong. Acta Petrol Sin 35(5):1566–1582(in Chinese with English abstract)

  • Mallmann G, Neill HSCO (2007) The effect of oxygen fugacity on the partitioning of re between crystals and silicate melt during mantle melting. Geochim Cosmochim Acta 71:2837–2857

    Article  Google Scholar 

  • Mallmann G, Neill HSCO (2009) The crystal/melt partitioning of V during mantle melting as a function of oxygen fugacity compared with some other elements (Al, P, ca, Sc, Ti, Cr, Fe, Ga, Y, Zr and Nb). J Petrol 50:1765–1794

    Article  Google Scholar 

  • Mao JW, Pirajno F, Cook N (2011) Mesozoic metallogeny in East China and corresponding geodynamic settings-An introduction to the special issue. Ore Geol Rev 43(1):1–7

    Article  Google Scholar 

  • Nash WM, Smythe DJ, Wood BJ (2019) Compositional and temperature effects on sulfur speciation and solubility in silicate melts. Earth Planet Sci Lett 507:187–198

    Article  Google Scholar 

  • Nimis P, Taylor WR (2000) Single clinopyroxene thermobarometry for garnet peridotites. Part I. calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer. Contrib Mineral Petrol 139:541–554

    Article  Google Scholar 

  • Ning SY, Wang FY, Xue WD, Zhou TF (2017) Geochemistry of the Baoshan pluton in the Tongling region of the lower Yangtze River belt. Geochimica 46(5):397–412 (in Chinese with English abstract)

    Google Scholar 

  • Pearce JA, Stern RJ (2006) Origin of back-arc basin magmas: trace element and isotope perspectives. In: Christie DM, fisher CR, Lee SM and givens S (eds.). Back-arc spreading systems: geological, biological, chemical, and physical interactions. Washington, DC: American Geophysical Union 166:63–86

    Google Scholar 

  • Perinelli C, Giovanni BA, Aida MC, Roberta O, Pietro A (2012) Redox state of subcontinental lithospheric mantle and relationships with metasomatism: insights from spinel peridotites from northern Victoria land (Antarctica). Contrib Mineral Petrol 164:1053–1067

    Article  Google Scholar 

  • Ridolfi F, Puerini M, Renzulli A, Menna M, Toulkeridis T (2008) The magmatic feeding system of El Reventador volcano (SubAndean zone, Ecuador) constrained by texture, mineralogy and thermobarometry of the 2002 erupted products. J Volcanol Geoth Res 176:94–106

    Article  Google Scholar 

  • Ridolfi F, Renzulli A, Puerini M (2010) Stability and chemical equilibrium of amphibole in calc-alkaline magmas: an overview, new thermobarometric formulations and application to subduction-related volcanoes. Contrib Mineral Petrol 160:45–66

    Article  Google Scholar 

  • Ruprecht P, Wörner G (2007) Variable regimes in magma systems documented in plagioclase zoning patterns: El Misti stratovolcano and Andahua monogenetic cones. J Volcanol Geoth Res 165:142–162

    Article  Google Scholar 

  • Rollinson HR (1993) Using geochemical data: evaluation, presentation, interpretation. Mineral Mag 58(392):523–523

    Google Scholar 

  • Rudnick LR, Fountain DM (1995) Nature and composition of the continental crust: a lower crustal perspective. Rev Geophys 33:267–309

  • Scaillet B, Evans BW (1999) The 15 June 1991 eruption of mount Pinatubo; I, phase equilibria and pre-eruption P-T-fO2-fH2 conditions of the dacite magmas. J Petrol 40:381–411

    Article  Google Scholar 

  • Schumacher JC (2001) Institut für Mineralogie-Petrologie-Geochemie der Albert-Ludwigs. Acta Petrol Mineral 20(2):189–198

    Google Scholar 

  • Shu YC, Nielsen SG, Zeng ZG, Shinjo R, Blusztajn J, Wang XY, Chen S (2017) Tracing subducted sediment inputs to the Ryukyu arc-Okinawa trough system: evidence from thallium isotopes. Geochim Cosmochim Acta 217:462–491

    Article  Google Scholar 

  • Smart KA, Tappe S, Simonetti A, Simonetti SS, Woodland AB, Harris C (2017) Tectonic significance and redox state of Paleoproterozoic eclogite and pyroxenite components in the slave cratonic mantle lithosphere, voyageur kimberlite, Arctic Canada. Chem Geol 455:98–119

    Article  Google Scholar 

  • Smith VJ (1974) Feldspar minerals. Tom 2. Chemical and textural properties. Springer-Verlag

  • Spear FS (1981) Amphibole-plagioclase equilibria: An empirical model for the relation albite+tremolite=edenite+4 quartz. Contrib Mineral Petrol 77:355–364

    Article  Google Scholar 

  • Tatsumi Y (2000) Continental crust formation by crustal delamination in subduction zones and complementary accumulation of the enriched mantle I component in the mantle. Geochem Geophys Geosyst 1(12):1053

    Article  Google Scholar 

  • Tomkins AG, Rebryna KC, Weinberg RF, Schaefer BF (2012) Magmatic sulfde formation by reduction of oxidized arc basalt. J Petrol 53:1537–1567

    Article  Google Scholar 

  • Tso JL, Gilbert MC, Craig JR (1979) Sulfidation of synthetic biotites. Am Mineral 64(3–4):304–316

    Google Scholar 

  • Uchida E, Endo S, Makino M (2007) Relationship between solidification depth of granitic rocks and formation of hydrothermal ore deposits. Resour Geol 57(1):47–56

    Article  Google Scholar 

  • Wang CM, Deng J, Santosh M, Carranza EJM, Gong QJ, Guo CY, Xia R, Lai XR (2015) Timing, tectonic implications and genesis of gold mineralization in the Xincheng gold deposit, China: C-H-O isotopes, pyrite Rb-Sr and zircon fission track thermochronometry. Ore Geol Rev 65:659–673

    Article  Google Scholar 

  • Wang FY, Ge C, Ning SY, Nie LQ, Zhong GX, White NC (2017) A new approach to LA-ICP-MS mapping and application in geology. Acta Petrol Sin 33(11):3422–3436 (in Chinese with English abstract)

    Google Scholar 

  • Wang Y, Zhou LY, Liu SF, Li JY, Yang TN (2018) Post-cratonization deformation processes and tectonic evolution of the North China Craton. Earth-Sci Rev 177:320–365

  • Weatherley DK, Henley RW (2013) Flash vaporization during earthquakes evidenced by gold deposits. Nat Geosci 6(4):294–298

    Article  Google Scholar 

  • Xie YW, Zhang YQ (1990) Peculiarities and genetic significance of hornblende of hornblende from granite in the hengduansan region. Acta Mineral Sin 1:35–45 (in Chinese with English abstract)

    Google Scholar 

  • Xu YG (1993) Geothermometers applicable to the mantle xenoliths. Acta Petrol Sin 9(2):167–180 (in Chinese with English abstract)

    Google Scholar 

  • Yang KF, Fan HR, Santosh M, Hu FF, Wilde SA, Lan TG, Lu LN, Liu YS (2012) Reactivation of the Archean lower crust: implications for zircon geochronology, elemental and Sr-Nd-Hf isotopic geochemistry of late Mesozoic granitoids from northwestern Jiaodong terrane, the North China Craton. Lithos 146-147:112–127

  • Yang LQ, Deng J, Wang ZL, Guo LN, Li RH, Groves DI, Danyushevsky LV, Zhang C, Zheng XL, Zhao H (2016) Relationships between gold and pyrite at the Xincheng gold deposit, Jiaodong Peninsula, China: implications for gold source and deposition in a brittle epizonal environment. Econ Geol 111(1):105–126

  • Zhang L, Ren ZY, Nichols ARL, Zhang YH, Zhang Y, Qian SP, Liu JQ (2014) Lead isotope analysis of melt inclusions by LA-MC-ICP-MS. J Anal Atom Spectrom 29(8):1393–1405

    Article  Google Scholar 

  • Zhang L, Ren ZY, Wu YD, Li N (2018) Sr isotope measurement of basaltic glasses by LA-MC-ICP-MS based on a linear relationship between analytical bias and Rb/Sr ratios. Rapid Commun Mass Sp 32(2):105–112

    Article  Google Scholar 

  • Zhang ZK, Ling M, Zhang LP, Sun SJ, Sun WD (2020) High oxygen fugacity magma: implication for the destruction of the North China Craton. Acta Geochimica 39(2):161–171

  • 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

  • Zindler A, Hart S (1986) Chemical geodynamics. Annu Rev Earth Pl Sc 14:493–571

    Article  Google Scholar 

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Acknowledgements

Constructive comments of two anonymous reviewers and editor Qiuli Li are gratefully acknowledged. This research was financially supported by the National Key Research and Development Program of China (2020YFA0714802), the National Natural Science Foundation of China (41230311), and the Fundamental Research Funds for the Central Universities (grant FRF-TP-19-023A1).

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  1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 100083, No.29, Xueyuan Road, Haidian District, Beijing, People’s Republic of China

    Yao Ma & Xuefei Liu

  2. School of Civil and Resource Engineering, University of Science and Technology Beijing, 100083, No.30, Xueyuan Road, Haidian District, Beijing, People’s Republic of China

    Yayun Liang

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Ma, Y., Liu, X. & Liang, Y. Variation of oxygen fugacity during magmatic evolution: in-situ geochemistry of mafic dikes from Jiaodong, southeastern North China Craton. Miner Petrol 115, 577–593 (2021). https://doi.org/10.1007/s00710-021-00755-x

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