Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-25T08:10:03.326Z Has data issue: false hasContentIssue false
  • English
  • Français

Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing’an Range W belt, NE China: insights from the Narenwula Complex

Published online by Cambridge University Press:  10 January 2022

Wei Xie Open the ORCID record for Wei Xie [Opens in a new window] ,
Qing-Dong Zeng ,
Jin-Hui Yang ,
Rui Li ,
Zhuang Zhang ,
Rui-Liang Wang  and
Jin-Jian Wu
Wei Xie
Affiliation:
Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing100029, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China
Qing-Dong Zeng*
Affiliation:
Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing100029, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China
Jin-Hui Yang
Affiliation:
Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing100029, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China
Rui Li
Affiliation:
Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing100029, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China
Zhuang Zhang
Affiliation:
Chifeng Chaihulanzi Gold Mining Co. Ltd, Chifeng024000, China
Rui-Liang Wang
Affiliation:
Faculty of Geosciences and Resources, China University of Geosciences (Beijing), Beijing100083, China
Jin-Jian Wu
Affiliation:
Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing100029, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China
*
Author for correspondence: Qing-Dong Zeng, Email: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

Extensive magmatism in NE China, eastern Central Asian Orogenic Belt, has produced multi-stage granitic plutons and accompanying W mineralization. The Narenwula complex in the southwestern Great Xing’an Range provides important insights into the petrogenesis, geodynamic processes and relationship with W mineralization. The complex comprises granodiorites, monzogranites and granite porphyry. Mafic microgranular enclaves are common in the granodiorites, and have similar zircon U–Pb ages as their host rocks (258.5–253.9 Ma), whereas the W-bearing granitoids yield emplacement ages of 149.8–148.1 Ma. Permian granodiorites are I-type granites that are enriched in large-ion lithophile elements and light rare earth elements, and depleted in high field strength elements and heavy rare earth elements. Both the mafic microgranular enclaves and granodiorites have nearly identical zircon Hf isotopic compositions. The results suggest that the mafic microgranular enclaves and granodiorites formed by the mixing of mafic and felsic magmas. W-bearing granitoids are highly fractionated A-type granites, enriched in Rb, Th, U and Pb, and depleted in Ba, Sr, P, Ti and Eu. They have higher W concentrations and Rb/Sr ratios, and lower Nb/Ta, Zr/Hf and K/Rb ratios than the W-barren granodiorites. These data and negative ϵHf(t) values (–6.0 to –2.1) suggest that they were derived from the partial melting of ancient lower crust and subsequently underwent extreme fractional crystallization. Based on the regional geology, we propose that the granodiorites were generated in a volcanic arc setting related to the subduction of the Palaeo-Asian Ocean, whereas the W-bearing granitoids and associated deposits formed in a post-orogenic extensional setting controlled by the Mongol–Okhotsk Ocean and Palaeo-Pacific Ocean tectonic regimes.

Keywords

zircon U–Pb agesHf isotopesgeochemistryNarenwula complexGreat Xing’an RangeNE China
Type
Original Article
Information
Geological Magazine , Volume 159 , Issue 4 , April 2022 , pp. 593 - 627
Copyright
© The Author(s), 2022. 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

Abrajevitch, A, Zyabrev, S, Didenko, AN and Kodama, K (2012) Palaeomagnetism of the West Sakhalin Basin: evidence for northward displacement during the Cretaceous. Geophysical Journal International 190, 1439–54.10.1111/j.1365-246X.2012.05572.xCrossRefGoogle Scholar
Annen, C, Blundy, JD and Sparks, RSJ (2006) The genesis of intermediate and silicic magmas in deep crustal hot zones. Journal of Petrology 47, 505–39.10.1093/petrology/egi084CrossRefGoogle Scholar
Arevalo, RJ and McDonough, WF (2008) Tungsten geochemistry and implications for understanding the earth’s interior. Earth and Planetary Science Letters 272, 656–65.10.1016/j.epsl.2008.05.031CrossRefGoogle Scholar
Ballouard, C, Poujol, M, Boulvais, P, Branquet, Y, Tartese, R and Vigneresse, JL (2016) Nb–Ta fractionation in peraluminous granites: a marker of magmatic-hydrothermal transition. Geology 3, 231–4.10.1130/G37475.1CrossRefGoogle Scholar
Barbarin, B (2005) Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: nature, origin, and relations with the hosts. Lithos 88, 155–77.10.1016/j.lithos.2004.05.010CrossRefGoogle Scholar
Batchelor, RA and Bowden, VP (1985) Petrogenetic interpretation of granitoids rock series using multicationic parameters. Chemical Geology 48, 43–55.10.1016/0009-2541(85)90034-8CrossRefGoogle Scholar
Bau, M (1996) Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect. Contributions to Mineralogy and Petrology 123, 323–33.10.1007/s004100050159CrossRefGoogle Scholar
Bedard, JH (1990) Enclaves from the A-type granite of the Megantic Complex, White Mountain magma series: clues to granite magmagenesis. Journal of Geophysical Research 1990, 17797–819.10.1029/JB095iB11p17797CrossRefGoogle Scholar
Belousova, EA, Griffin, WL, O’Reilly, SY and Fisher, NI (2002) Igneous zircon: trace element composition as an indicator of source rock type. Contributions to Mineralogy and Petrology 143, 602–22.10.1007/s00410-002-0364-7CrossRefGoogle Scholar
Berzina, AP, Berzina, AN and Gimon, VO (2014) Geochemical and Sr–Pb–Nd isotopic characteristics of the Shakhtama porphyry Mo–Cu system (Eastern Transbaikalia, Russia). Journal of Asian Earth Sciences 79, 655–65.10.1016/j.jseaes.2013.07.028CrossRefGoogle Scholar
Bonin, B (2004) Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting mantle and crustal sources? A review. Lithos 78, 1–24.10.1016/j.lithos.2004.04.042CrossRefGoogle Scholar
Bonin, B (2007) A-type granites and related rocks: evolution of a concept, problems and prospects. Lithos 97, 1–29.10.1016/j.lithos.2006.12.007CrossRefGoogle Scholar
Bouvier, A, Vervoort, JD and Patchett, PJ (2008) The Lu–Hf and Sm–Nd isotopic composition of CHUR, constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth and Planetary Science Letters 273, 48–57.10.1016/j.epsl.2008.06.010CrossRefGoogle Scholar
Breiter, K, Müller, A, Leichmann, J and Gabašová, A (2005) Textural and chemical evolution of a fractionated granitic system: the Podlesí stock, Czech Republic. Lithos 80, 323–45.10.1016/j.lithos.2003.11.004CrossRefGoogle Scholar
Cao, JY, Wu, QH, Yang, XY, Deng, XT, Li, H, Kong, H and Xi, XS (2020) Geochemical factors revealing the differences between the Xitian and Dengfuxian composite plutons, middle Qin-Hang Belt: implications to the W–Sn mineralization. Ore Geology Reviews 118, 103353. doi: 10.1016/j.oregeorev.2020.103353.CrossRefGoogle Scholar
Cao, HH, Xu, WL, Pei, FP, Wang, ZW, Wang, F and Wang, ZJ (2013) Zircon U–Pb geochronology and petrogenesis of the Late Paleozoic–Early Mesozoic intrusive rocks in the eastern segment of the northern margin of the North China Block. Lithos 170–171, 191–207.10.1016/j.lithos.2013.03.006CrossRefGoogle Scholar
Cao, JY, Yang, XY, Du, JG, Wu, QH, Kong, H, Li, H, Wan, Q, Xi, XS, Gong, YS and Zhao, HR (2018) Formation and geodynamic implication of the Early Yanshanian granites associated with W–Sn mineralization in the Nanling range, South China: an overview. International Geology Review 60, 1744–71.10.1080/00206814.2018.1466370CrossRefGoogle Scholar
Castro, A, Patiño Douce, AE, Corretgé, LG, De La Rosa, JD, El-Biad, M and El-Hmidi, H (1999) Origin of peraluminous granites and granodiorites, Iberian Massif, Spain: an experimental test of granite petrogenesis. Contributions to Mineralogy and Petrology 135, 255–76.10.1007/s004100050511CrossRefGoogle Scholar
Chappell, BW (1996) Magma mixing and the production of compositional variation within granite suites: evidence from the granites of southeastern Australia. Journal of Petrology 37, 449–70.10.1093/petrology/37.3.449CrossRefGoogle Scholar
Chappell, BW (1999) Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites. Lithos 46, 535–51.10.1016/S0024-4937(98)00086-3CrossRefGoogle Scholar
Chappell, BW and White, AJR (1992) I-and S-type granites in the Lachlan Fold Belt. Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, 1–26.10.1017/S0263593300007720CrossRefGoogle Scholar
Chappell, BW, White, AJR and Wyborn, D (1987) The importance of residual source material in granite petrogenesis. Journal of Petrology 28, 1111–38.10.1093/petrology/28.6.1111CrossRefGoogle Scholar
Che, XD, Linnen, RL, Wang, RC, Aseri, A and Thibault, Y (2013) Tungsten solubility in evolved granitic melts: an evaluation of magmatic wolframite. Geochimica et Cosmochimica Acta 106, 84–98.10.1016/j.gca.2012.12.007CrossRefGoogle Scholar
Chen, B, Jahn, BM and Tian, W (2009) Evolution of the Solonker suture zone: constraints from zircon U–Pb ages, Hf isotopic ratios and whole-rock Sr–Nd isotope compositions of subduction and collision-related magmas and forearc sediments. Journal of Asian Earth Sciences 34, 245–57.CrossRefGoogle Scholar
Chen, B, Jahn, BM, Wilde, S and Xu, B (2000) Two contrasting Paleozoic magmatic belts in northern Inner Mongolia, China: petrogenesis and tectonic implications. Tectonophysics 328, 157–82.CrossRefGoogle Scholar
Chen, YD, Price, RC and White, AJR (1989) Inclusions in three S-type granites from southeastern Australia. Journal of Petrology 30, 1181–218.CrossRefGoogle Scholar
Chen, GZ, Wu, G, Li, TG, Liu, RL, Wu, LW, Zhang, PC, Zhang, T and Chen, YC (2018) LA-ICP-MS zircon and cassiterite U–Pb ages of Daolundaba copper-tungsten-tin deposit in Inner Mongolia and their geological significance. Mineral Deposits 37, 225–45 (in Chinese with English abstract).Google Scholar
Claiborne, LL, Miller, CF, Walker, BA, Wooden, JL, Mazdab, FK and Bea, F (2006) Tracking magmatic processes through Zr/Hf ratios in rocks and Hf and Ti zoning in zircons: an example from the Spirit Mountain batholith, Nevada. Mineralogical Magazine 70, 517–43.CrossRefGoogle Scholar
Clemens, JD, Holloway, JR and White, AJR (1986) Origin of an A-type granite: experimental constraints. American Mineralogist 71, 317–24.Google Scholar
Clemens, JD and Stevens, G (2012) What controls chemical variation in granitic magmas? Lithos 134–135, 317–29.CrossRefGoogle Scholar
Clemens, JD and Wall, VJ (1988) Controls on mineralogy of S-type volcanic and plutonic rocks. Lithos 21, 53–66.CrossRefGoogle Scholar
Collins, WJ, Beams, SD, White, AJR and Chappell, BW (1982) Nature and origin of A-type granites with particular reference to southeastern Australia. Contributions to Mineralogy and Petrology 80, 189–200.CrossRefGoogle Scholar
Collins, WJ, Wiebe, R, Healy, B and Richards, S (2006) Replenishment, crystal accumulation and floor aggradation in the megacrystic Kameruka Suite, Australia. Journal of Petrology 47, 2073–104.CrossRefGoogle Scholar
Deering, CD and Bachmann, O (2010) Trace element indicators of crystal accumulation in silicic igneous rocks. Earth and Planetary Science Letters 297, 324–31.CrossRefGoogle Scholar
Defant, MJ and Drummond, MS (1990) Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature 347, 662–5.CrossRefGoogle Scholar
Didier, J (1973) Granites and their Enclaves: The Bearing of Enclaves on the Origin of Granites. Amsterdam: Elsevier, 393 pp.Google Scholar
Dodge, FCW and Kistler, RW (1990) Some additional observations on inclusions in the granitic rocks of the Sierra Nevada. Journal of Geophysical Research: Solid Earth 95, 17841–48.CrossRefGoogle Scholar
Dostal, J and Chatterjee, AK (2000) Contrasting behavior of Nb/Ta and Zr/Hf ratios in a peraluminous granitic pluton (Nova Scotia, Canada). Chemical Geology 163, 207–18.CrossRefGoogle Scholar
Dostal, J, Kontak, DJ, Gerel, O, Gregory, SJ and Fayek, M (2015) Cretaceous ongonites (topaz-bearing albite-rich microleucogranites) from Ongon Khairkhan, Central Mongolia: products of extreme magmatic fractionation and pervasive metasomatic fluid: rock interaction. Lithos 236–237, 173–89.CrossRefGoogle Scholar
Eby, GN (1992) Chemical subdivision of the A-type granitoids: petrogenetic and tectonic implications. Geology 20, 641–44.2.3.CO;2>CrossRefGoogle Scholar
Eizenhöfer, PR, Zhao, GC, Zhang, J and Sun, M (2014) Final closure of the Paleo-Asian Ocean along the Solonker suture zone: constraints from geochronological and geochemical data of Permian volcanic and sedimentary rocks. Tectonics 33, 441–63.CrossRefGoogle Scholar
El Bouseily, AM and El Sokkary, AA (1975) The relation between Rb, Ba and Sr in granitic rocks. Chemical Geology 16, 207–19.CrossRefGoogle Scholar
Elburg, MA (1996) Evidence of isotopic equilibration between microgranitoid enclaves and host granodiorite, Warburton granodiorite, Lachlan Fold Belt, Australia. Lithos 38, 1–22.CrossRefGoogle Scholar
Fei, XH, Zhang, ZC, Cheng, ZG, Santosh, M, Jin, ZL, Wen, BB, Li, ZX and Xu, LJ (2018) Highly differentiated magmas linked with polymetallic mineralization: a case study from the Cuihongshan granitic intrusions, Lesser Xing’an Range, NE China. Lithos 302–303, 158–77.CrossRefGoogle Scholar
Feng, ZQ, Liu, YJ, Li, L, Jin, W, Jiang, LW, Li, WM, Wen, QB and Zhao, YL (2019) Geochemical and geochronological constraints on the tectonic setting of the Xinlin ophiolite, northern Great Xing’an Range, NE China. Lithos 326–327, 213–29.CrossRefGoogle Scholar
Fogliata, AS, Baez, MA, Hagemann, SG, Santos, JO and Sardi, F (2012) Post-orogenic, Carboniferous granite-hosted Sn–W mineralization in the Sierras Pampeanas Orogen, Northwestern Argentina. Ore Geology Reviews 45, 16–32.CrossRefGoogle Scholar
Fritzell, EH, Bull, AL and Shephard, GE (2016) Closure of the Mongol-Okhotsk Ocean: insights from seismic tomography and numerical modelling. Earth and Planetary Science Letters 445, 1–12.CrossRefGoogle Scholar
Frost, BR, Barnes, CG, Collins, WJ, Arculus, RJ, Ellis, DJ and Frost, CD (2001) A geochemical classification for granitic rocks. Journal of Petrology 42, 2033–48.CrossRefGoogle Scholar
Gao, X, Zhou, Z, Breiter, K, Ouyang, H and Liu, J (2019) Ore-formation mechanism of the Weilasituo tin–polymetallic deposit, NE China: constraints from bulk-rock and mica chemistry, He–Ar isotopes, and Re–Os dating. Ore Geology Reviews 109, 163–83.CrossRefGoogle Scholar
Ge, WC, Lin, Q, Sun, DY, Wu, FY, Yuan, ZK, Li, WY, Chen, MZ and Yin, CX (1999) Geochemical characteristics of the Mesozoic basalts in Da Hinggan Ling: evidence of the mantle-crust interaction. Acta Petrologica Sinica 15, 396–406 (in Chinese with English abstract).Google Scholar
Gibert, F, Moine, B, Schott, J and Dandurand, JL (1992) Modeling of the transport and deposition of tungsten in the scheelite-bearing calc-silicate gneisses of the Montagne Noire, France. Contributions to Mineralogy and Petrology 112, 371–84.CrossRefGoogle Scholar
Gou, J, Sun, DY and Qin, Z (2019) Late Jurassic–Early Cretaceous tectonic evolution of the Great Xing’an Range: geochronological and geochemical evidence from granitoids and volcanic rocks in the Erguna Block, NE China. International Geology Review 61, 1842–63.CrossRefGoogle Scholar
Green, TH (1995) Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system. Chemical Geology 120, 347–59.CrossRefGoogle Scholar
Griffin, WL, Wang, X, Jackson, SE, Pearson, SE, O’Reilly, SY, Xu, XS and Zhou, XM (2002) Zircon chemistry and magma genesis, SE China: in-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes. Lithos 61, 237–69.CrossRefGoogle Scholar
Guan, QB, Liu, ZH, Wang, B, Wang, X, Wang, XA, Shi, Q and Chen, YS (2018) Middle Jurassic−Early Cretaceous tectonic evolution of the Bayanhushuo area, southern Great Xing’an Range, NE China: constraints from zircon U–Pb geochronological and geochemical data of volcanic and subvolcanic rocks. International Geology Review 60, 1883–905.CrossRefGoogle Scholar
Guo, F, Huang, MW and Zhao, L (2019) Nd–Hf–O isotopic evidence for subduction-induced crustal replacement in NE China. Chemical Geology 525, 125–42.CrossRefGoogle Scholar
Guo, ZJ, Li, JW, Chang, YL, Han, ZG, Dong, XZ, Yang, YC, Tian, J, She, HQ, Xiang, AP and Kang, YJ (2015) Genetic types and ore-forming geological significance of granites in the Honghuaerji scheelite deposit, Inner Mongolia. Acta Petrologica et Mineralogica 34, 322–42 (in Chinese with English abstract).Google Scholar
Guo, ZX, Yang, YT, Zyabrev, S and Hou, ZH (2017) Tectonostratigraphic evolution of the Mohe-upper Amur Basin reflects the final closure of the Mongol-Okhotsk Ocean in the latest Jurassic-earliest Cretaceous. Journal of Asian Earth Sciences 145, 494–511.CrossRefGoogle Scholar
Han, SJ, Wang, X, Wang, X, Wang, Y and Zhang, Y (2021) Geochronology and geochemistry of late Jurassic–Early Cretaceous volcanic rocks in the southern Great Xing’an range, NE China: constraints for late Mesozoic tectono-magmatic evolution. International Geology Review 63, 1366–88. doi: 10.1080/00206814.2020.1768442.CrossRefGoogle Scholar
Han, J, Zhou, JB, Wang, B and Cao, JL (2015) The final collision of the CAOB: constraint from the zircon U–Pb dating of the Linxi Formation, Inner Mongolia. Geoscience Frontiers 6, 211–25.CrossRefGoogle Scholar
Harlaux, M, Mercadier, J, Marignac, C, Peiffert, C, Cloquet, C and Cuney, M (2018) Tracing metal sources in peribatholitic hydrothermal W deposits based on the chemical composition of wolframite: the example of the Variscan French Massif Central. Chemical Geology 479, 58–85.CrossRefGoogle Scholar
Harris, NB, Pearce, JA and Tindle, AG (1986) Geochemical characteristics of collision-zone magmatism. In Collision Tectonics (eds Coward, MP and Reis, AC), pp. 67–81. Geological Society of London, Special Publication no. 19.Google Scholar
He, XH, Tan, SC, Liu, Z, Bai, ZJ, Wang, XC, Wang, YC and Zhong, H (2020) Petrogenesis of the Early Cretaceous Aolunhua adakitic monzogranite porphyries, Southern Great Xing’an Range, NE China: implication for geodynamic setting of Mo mineralization. Minerals 10, 332–52.CrossRefGoogle Scholar
Hirose, K (1997) Melting experiments on Iherzolite KLB-1 under hydrous conditions and generation of high-magnesian andesitic melts. Geology 25, 42–4.2.3.CO;2>CrossRefGoogle Scholar
Hou, KJ, Li, YH, Zou, TR, Qu, XM, Shi, YR and Xie, GQ (2007) Laser ablation-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geological applications. Acta Petrologica Sinica 23, 2595–604 (in Chinese with English abstract).Google Scholar
Hu, XL, Ding, ZJ, He, MC, Yao, SZ, Zhu, BP, Shen, J and Chen, B (2014) Two epochs of magmatism and metallogeny in the Cuihongshan Fe-polymetallic deposit, Heilongjiang Province, NE China: constrains from U–Pb and Re–Os geochronology and Lu–Hf isotopes. Journal of Geochemical Exploration 143, 116–26.CrossRefGoogle Scholar
Huang, LC and Jiang, SY (2014) Highly fractionated S-type granites from the giant Dahutang tungsten deposit in Jiangnan orogen, southeast China: geochronology, petrogenesis and their relationship with W-mineralization. Lithos 202–203, 207–26.CrossRefGoogle Scholar
Huang, JL and Zhao, DP (2006) High-resolution mantle tomography of China and surrounding regions. Journal of Geophysical Research 111, B09305. doi: 10.1029/2005JB004066.CrossRefGoogle Scholar
IMBGMED (Inner Mongolian Bureau of Geology and Mineral Exploration and Development) (2016) Prospecting Report of Narenwula W-Bi-Ag Polymetallic Deposit at Xianghuang Banner, Inner Mongolia Autonomous Region County. Beijing: Geological Publishing House, 265 pp. (in Chinese).Google Scholar
IMBGMR (Inner Mongolian Bureau of Geology Mineral Resources) (1991) Regional Geology of Inner Mongolia. Beijing: Geological Publishing House, 725 pp. (in Chinese).Google Scholar
Jiang, SH, Bagas, L, Hu, P, Han, N, Chen, CL, Liu, Y and Kang, H (2016) Zircon U–Pb ages and Sr–Nd–Hf isotopes of the highly fractionated granite with tetrad REE patterns in the Shamai tungsten deposit in eastern Inner Mongolia, China: implications for the timing of mineralization and ore genesis. Lithos 261, 322–39.CrossRefGoogle Scholar
Jiang, SH, Chen, CL, Bagas, L, Liu, Y, Han, N, Kang, H and Wang, ZH (2017) Two mineralization events in the Baiyinnuoer Zn–Pb deposit in Inner Mongolia China: evidence from field observations, S–Pb isotopic compositions and U–Pb zircon ages. Journal of Asian Earth Sciences 144, 339–67.CrossRefGoogle Scholar
Jiang, H, Jiang, SY, Li, WQ, Zhao, KD and Peng, NJ (2018) Highly fractionated Jurassic I-type granites and related tungsten mineralization in the Shirenzhang deposit, northern Guangdong, south China: evidence from cassiterite and zircon U–Pb ages, geochemistry and Sr–Nd–Pb–Hf isotopes. Lithos 312–313, 186–203.CrossRefGoogle Scholar
Ji, Z, Ge, WC, Yang, H, Wang, QH, Zhang, YL, Wang, ZH and Bi, JH (2018) Late Jurassic rhyolites from the Wuchagou region in the central Great Xing’an Range, NE China: petrogenesis and tectonic implications. Journal of Asian Earth Sciences 158, 381–97.CrossRefGoogle Scholar
Ji, D, Liu, HC and Li, YL (2020) Large-scale early Cretaceous lower-crust melting derived adakitic rocks in NE China: implications for convergent bidirectional subduction and slab rollback. International Geology Review 62, 2324–43. doi: 10.1080/00206814.2019.1697968.CrossRefGoogle Scholar
Ji, Z, Meng, QA, Wan, CB, Zhu, DF, Ge, WC, Zhang, YL, Yang, H and Dong, Y (2019) Geodynamic evolution of flat-slab subduction of Paleo-Pacific Plate: constraints from Jurassic adakitic lavas in the Hailar Basin, NE China. Tectonics 38, 4301–19.CrossRefGoogle Scholar
Jing, JH, Yang, H, Ge, WC, Dong, Y, Ji, Z, Jing, Y, Bi, JH and Zhou, HY (2021) Early Cretaceous crust–mantle interaction linked to rollback of the Palaeo-Pacific flat-subducting slab: constraints from the intermediate–felsic volcanic rocks of the northern Great Xing’an Range, NE China. Geological Magazine 158, 1617–38.CrossRefGoogle Scholar
Ju, W and Hou, G (2014) Late Permian to Triassic intraplate orogeny of the southern Tianshan and adjacent regions, NW China. Geoscience Frontiers 5, 83–93.CrossRefGoogle Scholar
Keppler, H and Wyllie, PJ (1991) Partitioning of Cu, Sn, Mo, W, U, and Th between melt and aqueous fluid in the systems haplogranite-H2O-HCl and haplogranite-H2O-HF. Contributions to Mineralogy and Petrology 109, 139–50.CrossRefGoogle Scholar
Kerr, A and Fryer, BJ (1993) Nd isotopic evidence for crust–mantle interaction in the generation of A-type granitoid suites in Labrador, Canada. Chemical Geology 104, 39–60.CrossRefGoogle Scholar
Khanchuk, AI (2001) Pre-Neogene tectonics of the Sea-of-Japan regions: a view from the Russian side. Earth Science 55, 275–91.Google Scholar
King, PL, White, AJR, Chappell, W and Allen, CM (1997) Characterization and origin of aluminous A-type granites from the Lachlan Fold Belt, Southeastern Australia. Journal of Petrology 38, 371–91.CrossRefGoogle Scholar
Klemme, S and O’Neill, HS (2000) The near-solidus transition from garnet lherzolite to spinel lherzolite. Contributions to Mineralogy and Petrology 138, 237–48.CrossRefGoogle Scholar
Kravchinsky, VA, Cogné, JP, Harbert, WP and Kuzmin, MI (2002) Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia. Geophysical Journal International 148, 34–57.CrossRefGoogle Scholar
Lehmann, B (1987) Tin granites, geochemical heritage, magmatic differentiation. Geologische Rundschau 76, 177–85.CrossRefGoogle Scholar
Lehmann, B, Ishihara, S, Michel, H, Miller, J, Rapela, C, Sanchez, A, Tistl, M and Winkelmann, L (1990) The Bolivian tin province and regional tin distribution in the Central Andes: a reassessment. Economic Geology 85, 1044–58.CrossRefGoogle Scholar
Li, S, Chung, SL, Wang, T, Wilde, SA, Chu, MF and Guo, QQ (2017) Tectonic significance and geodynamic processes of large-scale Early Cretaceous granitoids magmatic events in the southern Great Xing’an Range, North China. Tectonics 36, 615–33.CrossRefGoogle Scholar
Li, R, Collins, WJ, Yang, JH, Blereau, E and Wang, H (2021) Two-stage hybrid origin of Lachlan S-type magmas: a re-appraisal using isotopic microanalysis of lithic inclusion minerals. Lithos 402–403, 106378. doi: 10.1016/j.lithos.2021.106378.CrossRefGoogle Scholar
Li, Y, Ding, LL, Xu, WL, Wang, F, Tang, J, Zhao, S and Wang, ZJ (2015) Geochronology and geochemistry of muscovite granite in Sunwu area, NE China: implications for the timing of closure of the Mongol-Okhotsk Ocean. Acta Petrologica Sinica 31, 56–66 (in Chinese with English abstract).Google Scholar
Li, JJ, Fu, C, Tang, WL, Li, HM, Lin, YX, Zhang, T, Wang, SG, Zhao, ZL, Dang, ZC and Zhao, LJ (2016) The metallogenic age of the Shamai wolframite deposit in Dong Ujimqin Banner, Inner Mongolia. Geological Bulletin of China 35, 524–30 (in Chinese with English abstract).Google Scholar
Li, PW, Gao, R, Guan, Y and Li, QS (2006) Palaeomagnetic constraints on the final closure time of Solonker-Linxi suture. Journal of Jilin University (Earth Science Edition) 36, 744–58 (in Chinese with English abstract).Google Scholar
Li, J, Huang, XL, Fu, Q and Li, WX (2021) Tungsten mineralization during the evolution of a magmatic-hydrothermal system: mineralogical evidence from the Xihuashan rare-metal granite in South China. American Mineralogist 106, 443–60.CrossRefGoogle Scholar
Li, SZ, Suo, YH, Li, XY, Zhou, J, Santosh, M, Wang, PC, Wang, GZ, Guo, LL, Yu, SY, Lan, HY, Dai, LM, Zhou, ZZ, Cao, XZ, Zhu, JJ, Liu, B, Jiang, SH, Wang, G and Zhang, GW (2019) Mesozoic tectono-magmatic response in the East Asian ocean-continent connection zone to subduction of the Paleo-Pacific Plate. Earth-Science Reviews 192, 91–137.CrossRefGoogle Scholar
Li, S, Wilde, SA, He, ZJ, Jiang, XJ, Liu, RY and Zhao, L (2014) Triassic sedimentation and postaccretionary crustal evolution along the Solonker suture zone in Inner Mongolia, China. Tectonics 33, 960–81.CrossRefGoogle Scholar
Li, YS, Yu, XF, Mi, KF, Carranza, EJM, Liu, JJ, Jia, WB and He, S (2019) Deposit geology, geochronology and geochemistry of the Gongpengzi skarn Cu–Zn–W polymetallic deposit, NE China. Ore Geology Reviews 109, 465–81.CrossRefGoogle Scholar
Li, YL, Zhou, HW, Brouwer, FM, Xiao, WJ, Wijbrans, JR, Zhao, JH, Zhong, ZQ and Liu, HF (2014) Nature and timing of the Solonker suture of the Central Asian Orogenic Belt: insights from geochronology and geochemistry of basic intrusions in the Xilin Gol Complex, Inner Mongolia, China. International Journal of Earth Sciences 103, 41–60.CrossRefGoogle Scholar
Linnen, RL and Keppler, H (1997) Columbite solubility in granitic melts: consequences for the enrichment and fractionation of Nb and Ta in the Earth’s crust. Contributions to Mineralogy and Petrology 128, 213–27.CrossRefGoogle Scholar
Linnen, RL and Keppler, H (2002) Melt composition control of Zr/Hf fractionation in magmatic processes. Geochimica et Cosmochimica Acta 66, 3293–301.CrossRefGoogle Scholar
Linnen, RL and Williams-Jones, AE (1995) Genesis of a magmatic metamorphic hydrothermal system; the Sn–W polymetallic deposits at Pilok, Thailand. Economic Geology 90, 1921–35.CrossRefGoogle Scholar
Litvinovsky, BA, Jahn, BM and Eyal, M (2015) Mantle-derived sources of syenites from the A-type igneous suites-new approach to the provenance of alkaline silicic magmas. Lithos 232, 242–65.CrossRefGoogle Scholar
Liu, ZH (2009) Geological characteristic and origin of deposit in Cuihongshan W, Mo, Zn polymetallic deposit. M.Sc. thesis, Jilin University, Changchun, China. Published thesis (in Chinese with English abstract).Google Scholar
Liu, C, Deng, JF, Kong, WQ, Xu, LQ, Zhao, GC, Luo, ZH and Li, N (2011) LA-ICP-MS zircon U–Pb geochronology of the fine-grained granite and molybdenite Re–Os dating in the Wurinitu molybdenum deposit, Inner Mongolia, China. Acta Geologica Sinica (English Edition) 85, 1057–66.CrossRefGoogle Scholar
Liu, YS, Gao, S, Hu, ZC, Gao, CG, Zong, KQ and Wang, DB (2010) Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U–Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology 51, 537–71.CrossRefGoogle Scholar
Liu, YF, Jiang, SH and Bagas, L (2016) The genesis of metal zonation in the Weilasituo and Bairendaba Ag–Zn–Pb–Cu–(Sn–W) deposits in the shallow part of a porphyry Sn–W–Rb system, Inner Mongolia, China. Ore Geology Reviews 75, 150–73.CrossRefGoogle Scholar
Liu, Y, Jiang, SH, Bagas, L, Chen, CL, Han, N and Wan, YY (2020) Petrogenesis and metallogenic potential of the Wulanba granite, southern Great Xing’an Range, NE China: constraints from whole-rock and apatite geochemistry. Geological Magazine 157, 411–34.CrossRefGoogle Scholar
Liu, YJ, Li, WM, Feng, ZQ, Wen, QB, Neubauer, F and Liang, CY (2017) A review of the Paleozoic tectonics in the eastern part of Central Asian Orogenic Belt. Gondwana Research 43, 123–48.CrossRefGoogle Scholar
Liu, CH and Nie, FJ (2015) Permian magmatic sequences of the Bilihe gold deposit in central Inner Mongolia, China: petrogenesis and tectonic significance. Lithos 231, 35–52.CrossRefGoogle Scholar
Liu, LJ and Stegman, DR (2012) Origin of Columbia River flood basalt controlled by propagating rupture of the Farallon slab. Nature 482, 386–9.CrossRefGoogle ScholarPubMed
Liu, RL, Wu, G, Li, TG, Chen, GZ, Wu, LW, Zhang, PC, Zhang, T, Jiang, B and Liu, WY (2018) LA-ICP-MS cassiterite and zircon U–Pb ages of the Weilasituo tin-polymetallic deposit in the southern Great Xing’an Range and their geological significance. Earth Science Frontiers 25, 183–201 (in Chinese with English abstract).Google Scholar
Liu, CF, Zhou, ZG, Tang, YJ, Wu, C, Li, HY, Zhu, Y, Jiang, T, Liu, WC and Ye, BY (2017) Geochronology and tectonic settings of Late Jurassic – Early Cretaceous intrusive rocks in the Ulanhot region, central and southern Da Xingan Range. Geological Magazine 154, 923–45.CrossRefGoogle Scholar
Ludwig, KR (2003) User’s Manual for Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication no. 4, 70 pp.Google Scholar
Ma, XH, Zhu, WP, Zhou, ZH and Qiao, SL (2017) Transformation from Paleo-Asian Ocean closure to Paleo-Pacific subduction: new constraints from granitoids in the eastern Jilin-Heilongjiang Belt, NE China. Journal of Asian Earth Sciences 144, 261–86.CrossRefGoogle Scholar
Maas, R, Nicholls, IA and Legg, C (1997) Igneous and metamorphic enclaves in the S-type Deddick granodiorite, Lachlan Fold Belt, SE Australia: petrographic, geochemical and Nd–Sr isotopic evidence for crustal melting and magma mixing. Journal of Petrology 38, 815–41.CrossRefGoogle Scholar
Maniar, PD and Piccoli, PM (1989) Tectonic discrimination of granitoids. Geological Society of America Bulletin 101, 635–43.2.3.CO;2>CrossRefGoogle Scholar
Mao, JW, Cheng, YB, Chen, MH and Franco, P (2013) Major types and time–space distribution of Mesozoic ore deposits in South China and their geodynamic settings. Mineralium Deposita 48, 267–94.Google Scholar
Mao, AQ, Sun, DY, Yang, DG, Tang, ZY, Zheng, H and Liu, Y (2020) Petrogenesis and tectonic implications of Early Cretaceous volcanic rocks from the Shanghulin Basin within the north-western Great Xing’an Range, NE China: constraints from geochronology and geochemistry. Geological Journal 55, 3476–96.CrossRefGoogle Scholar
Maruyama, S, Isozaki, Y, Kimura, G and Terabayashi, M (1997) Paleogeographic maps of the Japanese Islands: plate tectonic synthesis from 750 Ma to the present. Island Arc 6, 121–42.CrossRefGoogle Scholar
McDonough, WF and Sun, SS (1995) The composition of the earth. Chemical Geology 120, 223–53.CrossRefGoogle Scholar
Mei, W, Lu, XB, Liu, Z, Tang, RK, Ai, ZL, Wang, XD and Cisse, M (2015) Geochronological and geochemical constraints on the ore-related granites in Huanggang deposit, southern Great Xing’an Range, NE China and its tectonic significance. Geosciences Journal 19, 53–67.CrossRefGoogle Scholar
Mi, KF, Lü, ZC, Zhao, SJ, Yan, TJ, Yu, HY and Dong, SY (2021) Petrogenesis and metallogenic implications of the Late Jurassic Dagayin pluton, southern Great Xing’an Range, northeast China: integrated geochronological, petrological, and geochemical constraints. Journal of Geochemical Exploration 220, 106666. doi: 10.1016/j.gexplo.2020.106666.CrossRefGoogle Scholar
Middlemost, EAK (1994) Naming materials in the magma/igneous rock system. Earth-Science Reviews 37, 215–24.CrossRefGoogle Scholar
Mingram, B, Trumbull, RB, Littman, S and Gerstenberger, H (2000) A petrogenetic study of anorogenic felsic magmatism in the Cretaceous Paresis ring complex, Namibia: evidence for mixing of crust and mantle-derived components. Lithos 54, 1–22.CrossRefGoogle Scholar
Mushkin, A, Navon, O, Halicz, L, Hartmann, G and Stein, M (2003) The petrogenesis of A-type magmas from the Amram Massif, southern Israel. Journal of Petrology 44, 815–32.CrossRefGoogle Scholar
Ouyang, HG, Mao, JW, Zhou, ZH and Su, HM (2015) Late Mesozoic metallogeny and intracontinental magmatism, southern Great Xing’an Range, northeastern China. Gondwana Research 27, 1153–72.CrossRefGoogle Scholar
Pang, YM, Guo, XW, Zhang, XH, Zhu, XQ, Hou, FH, Wen, ZH and Han, ZZ (2020) Late Mesozoic and Cenozoic tectono-thermal history and geodynamic implications of the Great Xing’an Range, NE China. Journal of Asian Earth Sciences 189, 104155. doi: 10.1016/j.jseaes.2019.104155.CrossRefGoogle Scholar
Patiño Douce, AE (1999) What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas? In Understanding Granites: Integrating New and Classical Techniques (eds Castro, A, Fernandez, C and Vigneresse, JL), pp. 55–75. Geological Society of London, Special Publication no. 168.Google Scholar
Pearce, JA, Harris, NBW and Tindle, AG (1984) Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology 25, 956–83.CrossRefGoogle Scholar
Peccerillo, A and Taylor, SR (1976) Geochemistry of Eocene calc-alkaline volcanic rocks form the Kastamonu area, Northern Turkey. Contributions to Mineralogy and Petrology 58, 63–81.CrossRefGoogle Scholar
Plank, T (2005) Constraints from thorium/lanthanum on sediment recycling at subduction zones and the evolution of the continents. Journal of Petrology 46, 921–44.CrossRefGoogle Scholar
Qin, HF, Li, YF, Huang, C, Cai, SH and Ren, SM (2013) Palaeomagnetic investigation of Permian sandstone in Taohaiyingzi area of Inner Mongolia and its tectonic significance. Geological Bulletin of China 32, 388–98 (in Chinese with English abstract).Google Scholar
Qin, F, Liu, JM, Zeng, QD and Luo, ZH (2009) Petrogenetic and metallogenic mechanism of the Xiaodonggou porphyry molybdenum deposit in Hexigten Banner, Inner Mongolia. Acta Petrologica Sinica 25, 3357–68 (in Chinese with English abstract).Google Scholar
Rapp, PR and Watson, EB (1995) Dehydration melting of metabasalt at 8–32 kbar: implications for continental growth and crust-mantle recycling. Journal of Petrology 36, 891–931.CrossRefGoogle Scholar
Ren, YS, Niu, JP, Wang, H and Lei, E (2009) LA-ICP-MS zircon U–Pb age and its geological significance of tungsten-bearing Mengjialing granitic intrusion in Siping area, Jilin Province. Journal of Mineralogy and Petrology 29, 100–5 (in Chinese with English abstract).Google Scholar
Ren, Q, Zhang, S, Wu, H, Liang, Z, Miao, X, Zhao, H, Li, H, Yang, T, Pei, J and Davis, GA (2016) Further paleomagnetic results from the ∼155 Ma Tiaojishan Formation, Yanshan Belt, North China, and their implications for the tectonic evolution of the Mongol-Okhotsk suture. Gondwana Research 35, 180–91.CrossRefGoogle Scholar
Ribeiro, JM, Stern, RJ, Kelley, KA, Martinez, F, Ishizuka, O, Manton, WI and Ohara, Y (2013) Nature and distribution of slab-derived fluids and mantle sources beneath the Southeast Mariana forearc rift. Geochemistry, Geophysics, Geosystems 14, 4585–607.CrossRefGoogle Scholar
Romer, RL and Kroner, U (2016) Phanerozoic tin and tungsten mineralization—tectonic controls on the distribution of enriched protoliths and heat sources for crustal melting. Gondwana Research 31, 60–95.CrossRefGoogle Scholar
Romer, RL, Meixner, A and Förster, HJ (2014) Lithium and boron in late-orogenic granites – isotopic fingerprints for the source of crustal melts? Geochimica et Cosmochimica Acta 131, 98–114.CrossRefGoogle Scholar
Rudnick, RL and Gao, S (2003) Composition of the continental crust. In Treatise on Geochemistry, Vol. 3 (eds Holland, HD and Turekian, KK), pp. 1–64. Oxford: Elsevier-Pergamon.Google Scholar
Sarjoughian, F, Kananian, A, Haschke, M, Ahmadian, J, Ling, W and Zong, K (2012) Magma mingling and hybridization in the Kuh-e Dom pluton, Central Iran. Journal of Asian Earth Sciences 54–55, 49–63.CrossRefGoogle Scholar
Schaller, T, Dingwell, DB, Keppler, H, Knöller, W, Merwin, L and Sebald, A (1992) Fluorine in silicate glasses: a multinuclear nuclear magnetic resonance study. Geochimica et Cosmochimica Acta 56, 701–7.CrossRefGoogle Scholar
Sengör, AMC, Natal’in, BA and Burtman, VS (1993) Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature 364, 299–307.CrossRefGoogle Scholar
Shang, QH (2004) Occurrences of Permian radiolarians in central and eastern Nei Mongol (Inner Mongolia) and their geological significance to the Northern China Orogen. Chinese Science Bulletin 49, 2613–19.CrossRefGoogle Scholar
Shao, J, Li, XR and Yang, HZ (2011) Zircon SHRIMP U–Pb dating of granite in the Cuihongshan polymetallic deposit and its geological implications. Acta Geoscientica Sinica 32, 163–70 (in Chinese with English abstract).Google Scholar
Shao, JA, Zhang, LQ, Xiao, QH and Li, XB (2005) Rising of Da Hinggan Mts in Mesozoic: a possible mechanism of intracontinental orogeny. Acta Petrologica Sinica 21, 789–94 (in Chinese with English abstract).Google Scholar
Shi, YR, Liu, DY, Miao, LC, Zhang, FQ, Jian, P, Zhang, W, Hou, KJ and Xu, JY (2010) Devonian A-type granitic magmatism on the northern margin of the North China Craton: SHRIMP U–Pb zircon dating and Hf isotopes of the Hongshan granite at Chifeng, Inner Mongolia, China. Gondwana Research 17, 632–41.CrossRefGoogle Scholar
Shi, KT, Wang, KY, Ma, XL, Li, SD, Li, J and Wang, R (2020) Fluid inclusions, C–H–O–S–Pb isotope systematics, geochronology and geochemistry of the Budunhua Cu deposit, northeast China: implications for ore genesis. Geoscience Frontiers 11, 1145–61.CrossRefGoogle Scholar
Signorelli, S and Carroll, MR (2000) Solubility and fluid-melt partitioning of Cl in hydrous phonolitic melts. Geochimica et Cosmochimica Acta 64, 2851–62.CrossRefGoogle Scholar
Singh, SK and Singh, S (2001) Geochemistry and tungsten metallogeny of the Balda granite, Rajasthan, India. Gondwana Research 4, 487–95.CrossRefGoogle Scholar
Skjerlie, KP and Johnston, AD (1993) Vapor-absent melting at 10 kbar of a biotite- and amphibole-bearing tonalitic gneiss: implications for the generation of A-type granites. Geology 20, 263–6.2.3.CO;2>CrossRefGoogle Scholar
Söderlund, U, Patchett, PJ, Vervoort, JD and Isachsen, CE (2004) The 176Lu decay constant determined by Lu–Hf and U–Pb isotope systematics of Precambrian mafic intrusions. Earth and Planetary Science Letters 219, 311–24.CrossRefGoogle Scholar
Stein, HJ (2014) Dating and tracing the history of ore formation. In Treatise in Geochemistry (2nd Edition), Vol. 13 (eds Turekian, KK, Holland, HD and Scott, SD), pp. 88–118. Oxford: Elsevier-Pergamon.Google Scholar
Steiner, BM (2019) W and Li–Cs–Ta geochemical signatures in I-type granites – a case study from the Vosges Mountains, NE France. Journal of Geochemical Exploration 197, 238–50.CrossRefGoogle Scholar
Sun, YG, Li, BL, Sun, FY, Ding, QF, Wang, BY, Li, YJ and Wang, K (2020) Mineralization events in the Xiaokele porphyry Cu (–Mo) deposit, NE China: evidence from zircon U–Pb and K-feldspar Ar–Ar geochronology and petrochemistry. Resource Geology 70, 254–72.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.Google Scholar
Suo, YH, Li, SZ, Jin, C, Zhang, Y, Zhou, J, Li, XY, Wang, PC, Liu, Z, Wang, XY and Somerville, I (2019) Eastward tectonic migration and transition of the Jurassic–Cretaceous Andean-type continental margin along Southeast China. Earth-Science Reviews 196, 102884. doi: 10.1016/j.earscirev.2019.102884.CrossRefGoogle Scholar
Tang, ZY, Sun, DY, Mao, AQ, Yang, DG, Deng, CZ and Liu, Y (2019) Timing and evolution of Mesozoic volcanism in the central Great Xing’an Range, northeastern China. Geological Journal 54, 3737–54.CrossRefGoogle Scholar
Taylor, SR and McLennan, SM (1995) The geochemical evolution of the continental crust. Reviews of Geophysics 33, 241–65.CrossRefGoogle Scholar
Thomas, R, Förster, HJ, Rickers, K and Webster, JD (2005) Formation of extremely F-rich hydrous melt fractions and hydrothermal fluids during differentiation of highly evolved tin-granite magmas: a melt/fluid-inclusion study. Contributions to Mineralogy and Petrology 148, 582–601.CrossRefGoogle Scholar
Tindle, AG and Pearce, JA (1983) Assimilation and partial melting of continental crust: evidence from the mineralogy and geochemistry of autoliths and xenoliths. Lithos 16, 185–202.CrossRefGoogle Scholar
Tomurtogoo, O, Windley, BF, Kroner, A, Badarch, G and Liu, DY (2005) Zircon age and occurrence of the Adaatsag ophiolite and Muron shear zone, central Mongolia: constraints on the evolution of the Mongol–Okhotsk ocean, suture and orogen. Journal of the Geological Society, London 162, 197–229.CrossRefGoogle Scholar
Turner, S, Arnaud, N, Liu, J, Rogers, N, Hawkesworth, C, Harris, N, Kelley, S, Van Calsteren, P and Deng, W (1996) Post-collision, shoshonitic volcanism on the Tibetan Plateau: implications for convective thinning of the lithosphere and the source of ocean island basalts. Journal of Petrology 37, 45–71.CrossRefGoogle Scholar
Turner, SP, Foden, JD and Morrison, RS (1992) Derivation of some A-type magmas by fractionation of basaltic magma: an example from the Padthaway Ridge, South Australia. Lithos 28, 151–79.CrossRefGoogle Scholar
Vallance, J, Cathelineau, M, Marignac, C, Boiron, MC, Fourcade, S, Martineau, F and Fabre, C (2001) Microfracturing and fluid mixing in granites: W-(Sn) ore deposition at Vaulry (NW French Massif Central). Tectonophysics 336, 43–61.CrossRefGoogle Scholar
Vernon, RH (1984) Microgranitoid enclaves in granites-globules of hybrid magma quenched in a plutonic environment. Nature 309, 438–39.CrossRefGoogle Scholar
Vernon, RH (2014) Microstructures of microgranitoid enclaves and the origin of S-type granitoids. Australian Journal of Earth Sciences 61, 227–39.CrossRefGoogle Scholar
Vernon, RH, Etheridge, MA and Wall, VJ (1988) Shape and microstructure of microgranitoid enclaves: indicators of magma mingling and flow. Lithos 22, 1–11.CrossRefGoogle Scholar
Vindel, E, Lopez, JA, Boiron, MC, Cathelineau, M and Prieto, AC (1995) P-V-T-X -fO2 evolution from wolframite to sulphide depositional stages in intragranitic W-veins. An example from the Spanish Central System. European Journal of Mineralogy 7, 675–88.CrossRefGoogle Scholar
Wan, L, Lu, CD, Zeng, ZX, Mohammed, AS, Liu, ZH, Dai, QQ and Chen, KL (2019) Nature and significance of the late Mesozoic granitoids in the southern Great Xing’an range, eastern Central Asian Orogenic Belt. International Geology Review 61, 584–606.CrossRefGoogle Scholar
Wang, F, Bagas, L, Jiang, S and Liu, Y (2017) Geological, geochemical, and geochronological characteristics of Weilasituo Sn-polymetal deposit, Inner Mongolia, China. Ore Geology Reviews 80, 1206–29.CrossRefGoogle Scholar
Wang, CZ, Gao, Q, Ren, L, Chen, JW, Wang, WB and Zheng, DH (2019) Fluid inclusions, H-O isotope and metallogenic epoch of the Xin’antun W-Mo deposit in Jiaohe City, Jilin Province. Geology and Exploration 55, 673–84 (in Chinese with English abstract).Google Scholar
Wang, ZH, Ge, WC, Yang, H, Zhang, YL, Bi, JH, Tian, DX and Xu, WL (2015) Middle Jurassic oceanic island igneous rocks of the Raohe accretionary complex, northeastern China: petrogenesis and tectonic implications. Journal of Asian Earth Sciences 111, 120–37.CrossRefGoogle Scholar
Wang, T, Guo, L, Zhang, L, Yang, QD, Zhang, JJ, Tong, Y and Ye, K (2015) Timing and evolution of Jurassic–Cretaceous granitoid magmatisms in the Mongol-Okhotsk belt and adjacent areas, NE Asia: implications for transition from contractional crustal thickening to extensional thinning and geodynamic settings. Journal of Asian Earth Sciences 97, 365–92.CrossRefGoogle Scholar
Wang, T, Guo, L, Zheng, YD, Donskaya, T, Gladkochub, G, Zeng, LS, Li, J, Wang, YB and Mazukabzov, AM (2012) Timing and processes of Late Mesozoic mid-lower-crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton: mainly constrained by zircon U–Pb ages from metamorphic core complexes. Lithos 154, 315–45.CrossRefGoogle Scholar
Wang, L, Tang, L, Zhang, ST, Santosh, M, Pei, QM, Cao, HW and Liu, FG (2020) Genesis of the Yujiadian F–Pb–Zn–Ag deposit, Inner Mongolia, NE China: constraints from geochemistry, fluid inclusion, zircon geochronology and stable isotopes. Ore Geology Reviews 122, 103528. doi: 10.1016/j.oregeorev.2020.103528.CrossRefGoogle Scholar
Wang, Y, Xu, B, Cheng, SD, Liao, W, Shao, J and Wang, Y (2014) Zircon U–Pb dating of the mafic lava from Wudaoshimen, Hexigten, Inner Mongolia and its geological significance. Acta Petrologica Sinica 30, 2055–62 (in Chinese with English abstract).Google Scholar
Wang, RL, Zeng, QD, Zhang, ZC, Guo, YP and Lu, JH (2020) Fluid evolution, H–O isotope and Re–Os age of molybdenite from the Baiyinhan tungsten deposit in the Eastern Central Asian Orogenic Belt, NE China, and its geological significance. Minerals 10, 664.CrossRefGoogle Scholar
Wang, RL, Zeng, QD, Zhang, ZC, Zhou, LL and Qin, KZ (2021) Extensive mineralization in the eastern segment of the Xingmeng orogenic belt, NE China: a regional view. Ore Geology Reviews 135, 104204. doi: 10.1016/j.oregeorev.2021.104204.CrossRefGoogle Scholar
Wang, T, Zheng, Y, Zhang, J, Zeng, L, Donskaya, T, Guo, L and Li, J (2011) Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia: perspectives from metamorphic core complexes. Tectonics 30, 1–27.CrossRefGoogle Scholar
Wang, F, Zhou, XH, Zhang, LC, Ying, JF, Zhang, YT, Wu, FY and Zhu, RX (2006) Late Mesozoic volcanism in the Great Xing’an Range (NE China): timing and implications for the dynamic setting of NE Asia. Earth and Planetary Science Letters 251, 179–98.CrossRefGoogle Scholar
Watson, EB and Harrison, TM (1983) Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types. Earth and Planetary Science Letters 64, 295–304.CrossRefGoogle Scholar
Webster, JD and Holloway, JR (1988) Experimental constraints on the partitioning of Cl between topaz rhyolite melt and H2O and H2O+CO2 fluids: new implications for granitic differentiation and ore deposition. Geochimica et Cosmochimica Acta 52, 2091–105.CrossRefGoogle Scholar
Webster, J, Thomas, R, Förster, HJ, Seltmann, R and Tappen, C (2004) Geochemical evolution of halogen-enriched granite magmas and mineralizing fluids of the Zinnwald tin–tungsten mining district, Erzgebirge, Germany. Mineralium Deposita 39, 452–72.CrossRefGoogle Scholar
Wedepohl, KH (1995) The composition of the continental crust. Geochimica et Cosmochimica Acta 59, 1217–32.CrossRefGoogle Scholar
Wei, W, Lv, XB and Wang, XD (2021) The granite porphyry hidden in the Shuangjianzishan deposit, southern Great Xing’an Range, NE China: geochronology, isotope geochemistry and tectonic implications. Geological Magazine 158, 995–1009.CrossRefGoogle Scholar
Wei, W, Zou, T, Huang, XK, Jiang, BB, Zhu, XY and Wu, XY (2020) Petrogenesis of early Cretaceous granitoids in the southern Great Xing’an Range, NE China: constraints from the Haliheiba pluton. Geochemistry 80, 125608. doi: 10.1016/j.chemer.2020.125608.CrossRefGoogle Scholar
Whalen, JB, Currie, KL and Chappell, BW (1987) A-type granites: geochemical characteristics, discrimination and petrogenesis. Contributions to Mineralogy and Petrology 95, 407–19.CrossRefGoogle Scholar
White, RV, Tarney, J, Kerr, AC, Saunders, AD, Kempton, PD, Pringle, MS and Klaver, GT (1999) Modification of an oceanic plateau, Aruba, Dutch Caribbean: implications for the generation of continental crust. Lithos 46, 43–68.CrossRefGoogle Scholar
Wilde, SA (2015) Final amalgamation of the Central Asian Orogenic Belt in NE China: Paleo-Asian Ocean closure versus Paleo-Pacific plate subduction — a review of the evidence. Tectonophysics 662, 345–62.CrossRefGoogle Scholar
Wood, SA and Samson, IM (2000) The hydrothermal geochemistry of tungsten in granitoid environments: I. Relative solubilities of ferberite and scheelite as a function of T, P, pH, and m NaCl. Economic Geology 95, 143–82.CrossRefGoogle Scholar
Wu, FY, Lin, JQ, Wilde, SA, Zhang, XO and Yang, JH (2005) Nature and significance of the Early Cretaceous giant igneous event in eastern China. Earth and Planetary Science Letters 233, 103–19.CrossRefGoogle Scholar
Wu, FY, Sun, DY, Ge, WC, Zhang, YB, Grant, ML, Wilde, SA and Jahn, BM (2011) Geochronology of the Phanerozoic granitoids in northeastern China. Journal of Asian Earth Sciences 41, 1–30.CrossRefGoogle Scholar
Xiang, AP, Chen, YC, Bagas, L, She, HQ, Kang, YJ, Yang, WS and Li, CJ (2016) Molybdenite Re–Os and U–Pb zircon dating and genesis of the Dayana W–Mo deposit in eastern Ujumchin, Inner Mongolia. Ore Geology Reviews 78, 268–80.CrossRefGoogle Scholar
Xiang, AP, Chen, YC, She, HQ, Li, GM and Li, YX (2018) Chronology and geochemical characteristics of granite in Weilianhe of Inner Mongolia and its geological significance. Geology in China 45, 963–76 (in Chinese with English abstract).Google Scholar
Xiang, AP, Wang, YJ, Qin, DJ, She, HQ, Han, ZG, Guan, JD and Kang, YJ (2014) Metallogenic and diagenetic age of Honghuaerji tungsten polymetallic deposit in Inner Mongolia. Mineral Deposits 33, 428–39 (in Chinese with English abstract).Google Scholar
Xiao, WJ and Santosh, M (2014) The western Central Asian Orogenic Belt: a window to accretionary orogenesis and continental growth. Gondwana Research 25, 1429–44.CrossRefGoogle Scholar
Xie, W, Zeng, QD, Wang, RL, Wu, JJ, Zhang, ZM, Li, FC and Zhang, Z (2021) Spatial-temporal distribution and tectonic setting of Mesozoic W-mineralized granitoids in the Xing-Meng Orogenic Belt, NE China. International Geology Review, published online 30 August 2021. doi: 10.1080/00206814.2021.1961105.CrossRefGoogle Scholar
Xu, B, Charvet, J, Chen, Y, Zhao, P and Shi, GZ (2013) Middle Paleozoic convergent orogenic belts in western Inner Mongolia (China): framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt. Gondwana Research 23, 1342–64.CrossRefGoogle Scholar
Xu, WL, Pei, FP, Wang, F, Meng, E, Ji, WQ, Yang, DB and Wang, W (2013) Spatial-temporal relationships of Mesozoic volcanic rocks in NE China: constraints on tectonic overprinting and transformations between multiple tectonic systems. Journal of Asian Earth Sciences 74, 167–93.CrossRefGoogle Scholar
Xu, B, Zhao, P, Wang, YY, Liao, W, Luo, ZW, Bao, QZ and Zhou, YH (2015) The pre-Devonian tectonic framework of Xing’an-Mongolia orogenic belt (XMOB) in north China. Journal of Asian Earth Sciences 97, 183–96.CrossRefGoogle Scholar
Yang, H, Ge, WC, Zhao, GC, Dong, Y, Xu, WL, Ji, Z and Yu, JJ (2015) Late Triassic intrusive complex in the Jidong region, Jiamusi-Khanka Block, NE China: geochemistry, zircon U–Pb ages, Lu–Hf isotopes, and implications for magma mingling and mixing. Lithos 224–225, 143–59.CrossRefGoogle Scholar
Yang, WB, Niu, HC, Hollings, P, Zurevinski, SE and Li, NB (2017) The role of recycled oceanic crust in the generation of alkaline A-type granites. Journal of Geophysical Research: Solid Earth 122, 9775–83.CrossRefGoogle Scholar
Yang, F, Sun, J, Wang, Y, Fu, J, Na, F, Fan, Z and Hu, Z (2019) Geology, geochronology and geochemistry of Weilasituo Sn-polymetallic deposit in Inner Mongolia, China. Minerals 9, 1–28.CrossRefGoogle Scholar
Yang, ZH, Wang, JP, Liu, JJ, Wang, SG, Wang, QY, Kang, SG, Zhang, JX and Zhao, Y (2016) Geochronology and geochemistry of the Wurinitu granites in Inner Mongolia and their geological implications Geoscience 30, 528–40 (in Chinese with English abstract).Google Scholar
Yang, JH, Wu, FY, Chung, SL, Wilde, SA and Chu, MF (2004) Multiple sources for the origin of granites: geochemical and Nd–Sr isotopic evidence from the Gudaoling granite and its mafic enclaves, Northeast China. Geochimica et Cosmochimica Acta 68, 4469–83.CrossRefGoogle Scholar
Yang, JH, Wu, FY, Shao, JA, Wilde, SA, Xie, LW and Liu, XM (2006) Constrains on the timing of uplift of the Yanshan fold and thrust belt, North China. Earth and Planetary Science Letters 246, 336–52.CrossRefGoogle Scholar
Yuan, SD, Williams-Jones, AE, Mao, JW, Zhao, PL, Yan, C and Zhang, DL (2018) The origin of the Zhangjialong tungsten deposit, South China: implications for W–Sn mineralization in large granite batholiths. Economic Geology 113, 1193–208.CrossRefGoogle Scholar
Yuan, SD, Williams-Jones, AE, Romer, RL, Zhao, PL and Mao, JW (2019) Protolith-related thermal controls on the decoupling of Sn and W in Sn–W metallogenic provinces: insights from the Nanling region, China. Economic Geology 114, 1005–12.CrossRefGoogle Scholar
Zajacz, Z, Halter, WE, Pettke, T and Guillong, M (2008) Determination of fluid/melt partition coefficients by LA-ICPMS analysis of co-existing fluid and silicate melt inclusions: controls on element partitioning. Geochimica et Cosmochimica Acta 72, 2169–97.CrossRefGoogle Scholar
Zeng, QD, Liu, JM, Chu, SX, Wang, YB, Sun, Y, Duan, XX and Zhou, LL (2012) Mesozoic molybdenum deposits in the East Xingmeng orogenic belt, northeast China: characteristics and tectonic setting. International Geology Review 54, 1843–69.CrossRefGoogle Scholar
Zeng, QD, Liu, JM, Qin, F and Zhang, ZL (2010) Geochronology of the Xiaodonggou porphyry Mo deposit in northern margin of North China Craton. Resource Geology 60, 192–202.CrossRefGoogle Scholar
Zeng, QD, Qin, KZ, Liu, JM, Li, GM, Zhai, MG, Chu, SX and Guo, YP (2015a) Porphyry molybdenum deposits in the Tianshan–Xingmeng orogenic belt, northern China. International Journal of Earth Sciences 104, 991–1023.CrossRefGoogle Scholar
Zeng, QD, Sun, Y, Chu, SX, Duan, XX and Liu, JM (2015b) Geochemistry and geochronology of the Dongshanwan porphyry Mo–W deposit, Northeast China: implications for the Late Jurassic tectonic setting. Journal of Asian Earth Sciences 97, 472–85.CrossRefGoogle Scholar
Zhai, DG, Liu, JJ, Li, JM, Zhang, M, Li, BY, Fu, X, Jiang, HC, Ma, LJ and Qi, L (2016) Geochronological study of Weilasituo porphyry type Sn deposit in Inner Mongolia and its geological significance. Mineral Deposits 35, 1011–22 (in Chinese with English abstract).Google Scholar
Zhai, M and Santosh, M (2013) Metallogeny of the North China Craton: link with secular changes in the evolving Earth. Gondwana Research 24, 275–97.CrossRefGoogle Scholar
Zhang, ZJ, Cheng, QM, Yao, LQ, Bai, HS and Li, C (2016) Zircon U–Pb–Hf isotopic systematics and geochemistry of the granites in the Wurintu molybdenum deposit, Inner Mongolia, China: implications for tectonic setting and genetic type of mineralization. Acta Geologica Sinica (English Edition) 90, 2066–79.CrossRefGoogle Scholar
Zhang, JH, Ge, WC, Wu, FY, Wilde, SA, Yang, JH and Liu, XM (2008) Large-scale Early Cretaceous volcanic events in the northern Great Xing’an Range, Northeastern China. Lithos 102, 138–57.CrossRefGoogle Scholar
Zhang, C, Quan, JY, Zhang, YJ, Liu, ZH, Li, W, Wang, Y, Qian, C, Zhang, L and Ge, JT (2020) Late Mesozoic tectonic evolution of the southern Great Xing’an Range, NE China: evidence from whole-rock geochemistry, and zircon U–Pb ages and Hf isotopes from volcanic rocks. Lithos 362–363, 105409. doi: 10.1016/j.lithos.2020.105409.CrossRefGoogle Scholar
Zhang, GL, Xie, W, Wen, SQ, Gong, EP, Guo, RR and Tang, TQ (2020) Petrogenesis and tectonic implications of Late Mesozoic volcanic rocks in the northern and central Great Xing’an Range, NE China: constraints from geochronology and geochemistry. Geological Journal 55, 8282–308.CrossRefGoogle Scholar
Zhang, Y, Yang, JH, Chen, JY, Wang, H and Xiang, YX (2017) Petrogenesis of Jurassic tungsten-bearing granites in the Nanling Range, South China: evidence from whole-rock geochemistry and zircon U–Pb and Hf–O isotopes. Lithos 278–281, 166–80.CrossRefGoogle Scholar
Zhang, XB, Wang, KY, Wang, CY, Li, W, Yu, Q, Wang, YC, Li, JF, Wan, D and Huang, GH (2017) Age, genesis, and tectonic setting of the Mo–W mineralized Dongshanwan granite porphyry from the Xilamulun metallogenic belt, NE China. Journal of Earth Science 28, 433–46.CrossRefGoogle Scholar
Zhang, XH, Zhang, HF, Tang, YJ, Wilde, SA and Hu, ZC (2008) Geochemistry of Permian bimodal volcanic rocks from central Inner Mongolia, North China: implication for tectonic setting and Phanerozoic continental growth in Central Asian Orogenic Belt. Chemical Geology 249, 262–81.CrossRefGoogle Scholar
Zhang, SH, Zhao, Y, Ye, H, Hou, KJ and Li, CF (2012) Early Mesozoic alkaline complexes in the northern North China Craton: implications for cratonic lithospheric destruction. Lithos 155, 1–18.CrossRefGoogle Scholar
Zhao, HL (2014) Ore genesis and geodynamic settings of tungsten deposits in Eastern Jilin and Heilongjiang Provinces. Ph.D. thesis, Jinlin University, Changchun, China. Published thesis (in Chinese with English abstract).Google Scholar
Zhou, Y (2013) The mineralization of Sansheng W–Mo deposit in Huade, Inner Mongolia. M.Sc. thesis, Chinese Academy of Geological Science, Beijing, China. Published thesis (in Chinese with English abstract).Google Scholar
Zhao, GC, Sun, M, Wilde, SA and Li, SZ (2005) Late Archaean to Paleoproterozoic evolution of the North China Craton: key issues revisited. Precambrian Research 136, 177–202.CrossRefGoogle Scholar
Zhu, XY, Zhang, ZH, Fu, X, Li, BY, Wang, YL, Jiao, ST and Sun, YL (2016) Geological and geochemical characteristics of the Weilasito Sn–Zn deposit, Inner Mongolia. Geology in China 43, 188–208 (in Chinese with English abstract).Google Scholar
Zorin, YA (1999) Geodynamics of the western part of the Mongol-Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia. Tectonophysics 306, 33–56.CrossRefGoogle Scholar
Zorpi, MJ, Coulon, C, Orsini, JB and Cocirta, C (1989) Magma mingling, zoning and emplacement in calc-alkaline granitoid plutons. Tectonophysics 157, 315–29.CrossRefGoogle Scholar
Supplementary material: File

Xie et al. supplementary material

Xie et al. supplementary material 1

Download Xie et al. supplementary material(File)
File 63.6 KB
Supplementary material: File

Xie et al. supplementary material

Xie et al. supplementary material 2

Download Xie et al. supplementary material(File)
File 39.6 KB