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Petrogenesis and metallogenic potential of the Wulanba granite, southern Great Xing’an Range, NE China: constraints from whole-rock and apatite geochemistry

Published online by Cambridge University Press:  06 November 2019

Yuan Liu ,
Si-Hong Jiang ,
Leon Bagas ,
Chun-Liang Chen ,
Ning Han  and
Yun-Yang Wan Open the ORCID record for Yun-Yang Wan [Opens in a new window]
Yuan Liu
Affiliation:
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing102249, China MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China
Si-Hong Jiang*
Affiliation:
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China
Leon Bagas
Affiliation:
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China Centre for Exploration Targeting, The University of Western Australia, Crawley, WA6009, Australia
Chun-Liang Chen
Affiliation:
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China
Ning Han
Affiliation:
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China
Yun-Yang Wan*
Affiliation:
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing102249, China
*
Author for correspondence: Si-Hong Jiang and Yun-Yang Wan, Emails: jiangsihong1@163.com and wanyunyang@cup.edu.cn
Author for correspondence: Si-Hong Jiang and Yun-Yang Wan, Emails: jiangsihong1@163.com and wanyunyang@cup.edu.cn
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Abstract

The Wulanba granite, consisting of biotite monzogranite and syenogranite, is located in the southern part of the Great Xing’an Range, NE China. Whole-rock major- and trace-element geochemistry suggests the Wulanba granite is a high-K–shoshonitic, slightly peraluminous and highly differentiated I-type granite. The Sr–Nd–Hf isotopes indicate that it originated from partial melting of juvenile crust derived from the depleted mantle with a minor input of old crust. The relatively young T2DM and tDM2 ages indicate it was most likely derived from a Late Neoproterozoic to Early Palaeozoic source. We have demonstrated that the biotite monzogranite is the ore-related intrusion of the Haobugao Zn–Fe mineralization based on the following geological, geochronological and geochemical evidence: (1) the chalcopyrite/pyrite in the biotite monzogranite and the continuous mineralization of drill core ZK2508; (2) the consistence of the emplacement age of the biotite monzogranite (~141–140/138 Ma) with the skarn mineralization age (~142 Ma); and (3) the presence of rich ore-forming elements (Fe–Zn–Cu) in the biotite monzogranite, and the similar Pb compositions of the sulfides from the Haobugao deposit and the biotite monzogranite. Compared to the barren syenogranite, the fertile biotite monzogranite is more oxidized, while the edges of the apatite grains in the biotite monzogranite are more oxidized than the centres. The average F/Cl ratio of the fertile biotite monzogranite (~123.45) is much higher than that of the barren syenogranite (~73.98). We conclude that these differences reflect unique geochemical signatures, and the geochemical composition of the apatite can be used to infer the economic potential of granites.

Keywords

apatiteore-related rockSr–Nd–Pb–Hf isotopesgeochronologyWulanba graniteGreat Xing’an Range
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 3 , March 2020 , pp. 411 - 434
Copyright
© Cambridge University Press 2019

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References

Amelin, Y, Lee, DC, Halliday, AN and Pidgeon, RT (1999) Nature of the earth’s earliest crust from hafnium isotopes in single detrital zircon. Nature 399, 252–5.CrossRefGoogle Scholar
Ballard, JR, Palin, MJ and Campbell, IH (2002) Relative oxidation states of magmas inferred from Ce(IV)/Ce(III) in zircon: application to porphyry copper deposits of northern Chile. Contributions to Mineralogy and Petrology 144, 347–64.CrossRefGoogle Scholar
Ballouard, C, Poujol, M, Boulvais, P, Branquet, Y, Tartèse, R and Vigneresse, JL (2016) Nb–Ta fractionation in peraluminous granites: a marker of the magmatic-hydrothermal transition. Geology 44, 231–4.CrossRefGoogle Scholar
Bonin, B (2007) A-type granites and related rocks: evolution of a concept, problems and prospects. Lithos 97, 1–29.CrossRefGoogle Scholar
Boudreau, AE, Mathez, EA and McCallum, IS (1986) Halogen geochemistry of the Stillwater and Bushveld Complexes: evidence for transport of the platinum-group elements by Cl-rich fluids. Journal of Petrology 27, 967–86.CrossRefGoogle Scholar
Cai, JH, Yan, GH, Xiao, CD, Wang, GY, Mu, BL and Zhang, RH (2004) Nd, Sr, Pb isotopic characteristics of the Mesozoic intrusive rocks in the Taihang–Da Hinggan Mountains tectonomagmatic belt and their source region. Acta Petrologica Sinica 20, 1225–42.Google Scholar
Canals, A and Cardellach, E (1997) Ore lead and sulphur isotope pattern from the low temperature veins of the Catalonian Coastal Ranges (NE Spain). Mineralium Deposita 32, 243–9.CrossRefGoogle Scholar
Chakhmouradian, AR, Reguir, EP, Zaitsev, AN, Couëslan, C, Xu, C, Kynický, J, Mumin, AH and Yang, P (2017) Apatite in carbonatitic rocks: compositional variation, zoning, element partitioning and petrogenetic significance. Lithos 274, 188–213.CrossRefGoogle Scholar
Chappell, BW (1999) Aluminium saturation in I- and S- type granites and the characterization of fractionated haplogranites. Lithos 46, 535–51.CrossRefGoogle Scholar
Chappell, BW, Bryant, CJ, Wyborn, D, White, AJR and Williams, IS (1998) High- and low temperature I-type granites. Resource Geology 48, 225–35.CrossRefGoogle Scholar
Chappell, BW and White, AJR (2001) Two contrasting granite types: 25 years later. Australian Journal of Earth Sciences 48, 489–99.CrossRefGoogle Scholar
Chen, YJ and Fu, SG (1992) Mineralization of Gold Deposits in West Henan, China. Beijing: China Seismological Press, 234 pp. (in Chinese with English abstract).Google Scholar
Chen, B, Jahn, BM, Simon, W 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, YJ, Pirajno, F and Qi, JP (2005) Origin of gold metallogeny and sources of ore-forming fluids, Jiaodong province, eastern China. International Geology Review 47, 530–49.CrossRefGoogle Scholar
Chen, L, Yan, Z, Wang, ZQ and Wang, KM (2017) Characteristics of apatite from 160–140 Ma Cu(Mo) and Mo(W) deposits in East Qinling. Acta Geologica Sinica 91, 1925–42 (in Chinese with English abstract).Google Scholar
Chu, XL, Huo, WG and Zhang, X (2001) Sulfur, carbon and lead isotope studies of the Dajing polymetallic deposit in Linxi county, Inner Mongolia, China — implication for metallogenic elements from hypomagmatic source. Resource Geology 51, 333–44.CrossRefGoogle 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
Coulson, IM, Dipple, GM and Raudsepp, M (2001) Evolution of HF and HCl activity in magmatic volatiles of the gold-mineralized Emerald Lake pluton, Yukon Territory, Canada. Mineralium Deposita 36, 594–606.CrossRefGoogle Scholar
Defant, MJ and Drummond, MS (1990) Derivation of some modern are magmas by melting of young subducted lithosphere. Nature 347, 662–5.CrossRefGoogle Scholar
Ding, T, Ma, D, Lu, JJ and Zhang, R (2015) Apatite in granitoids related to polymetallic mineral deposits in southeastern Hunan province, Shi–Hang zone, China: implications for petrogenesis and metallogenesis. Ore Geology Reviews 69, 104–17.CrossRefGoogle Scholar
Doherty, AL, Webster, JD, Goldoff, BA and Piccoli, PM (2014) Partitioning behavior of chlorine and fluorine in felsic melt–fluid(s)–apatite systems at 50 MPa and 850–950 °C. Chemical Geology 384, 94–109.CrossRefGoogle Scholar
Elhlou, S, Belousova, E, Griffin, WL, Pearson, NJ and O’Reilly, SY (2006) Trace element and isotopic composition of GJ-red zircon standard by laser ablation. Geochimica et Cosmochimica Acta 70, A158.CrossRefGoogle Scholar
Ellis, DJ and Thompson, AB (1986) Subsolidus and partial melting reactions in the quartz excess CaO–MgO–Al2O3–SiO2–H2O system under water-excess and water deficient conditions to 10 kb: some implications for the origin of peraluminous melts from mafic rocks. Journal of Petrology 27, 91–121.CrossRefGoogle Scholar
Eugster, HP and Wones, DR (1962) Stability relations of the ferruginous biotite, Annite. Journal of Petrology 3, 82–9.CrossRefGoogle Scholar
Fujimaki, H (1986) Partition coefficients of Hf, Zr, and REE between zircon, apatite and liquid. Contributions to Mineralogy and Petrology 94, 42–5.CrossRefGoogle Scholar
Gao, S, Rudnick, RL, Carlson, RW, McDonough, WF and Liu, YS (2002) Re–Os evidence for replacement of ancient mantle lithosphere beneath the North China craton. Earth and Planetary Science Letters 198, 307–22.CrossRefGoogle Scholar
Gelman, SE, Deering, CD, Bachmann, O, Huber, C and Gutiérrez, FJ (2014) Identifying the crystal graveyards remaining after large silicic eruptions. Earth and Planetary Science Letters 403, 299–306.CrossRefGoogle Scholar
Green, TH (1980) Island arc and continent-building magmatism: a review of petrogenetic models based on experimental petrology and geochemistry. Tectonophysics 63, 367–85.CrossRefGoogle Scholar
Guo, F, Fan, WM, Gao, XF, Li, CW, Miao, LC, Zhao, L and Li, HX (2010) Sr–Nd–Pb isotope mapping of Mesozoic igneous rocks in NE China: constraints on tectonic framework and Phanerozoic crustal growth. Lithos 120, 563–78.CrossRefGoogle Scholar
Guo, F, Fan, WM, Li, CW, Gao, XF and Miao, LC (2009) Early Cretaceous highly positive ϵNd felsic volcanic rocks from the Hinggan Mountains, NE China: origin and implications for Phanerozoic crustal growth. International Journal of Earth Sciences 98, 1395–411.CrossRefGoogle Scholar
Halliday, AN, Davidson, JP, Hildreth, W and Holden, P (1991) Modelling the petrogenesis of high Rb/Sr silicic magmas. Chemical Geology 92, 107–14.CrossRefGoogle Scholar
Han, G, Liu, Y, Neubauer, F, Johann, G, Zhao, Y, Wen, Q, Li, W, Wu, L, Jiang, X and Zhao, L (2012) Provenance analysis of Permian sandstones in the central and southern Da Xing’an mountains, China: constraints on the evolution of the eastern segment of the Central Asian Orogenic Belt. Tectonophysics 580, 100–13.CrossRefGoogle Scholar
Han, BF, Wang, SG, Jahn, BM, Hong, DW, Kagami, H and Sun, YL (1997) Depleted mantle source for the Ulungur river A-type granites from North Xinjiang, China: geochemistry and Nd–Sr isotopic evidence, and implications for Phanerozoic crustal growth. Chemical Geology 138, 135–59.CrossRefGoogle Scholar
Heinhost, J, Lehmann, B, Ermolov, P, Serykh, V and Zhurutin, S (2000) Paleozoic crustal growth and metallogeny of Central Asia: evidence from magmatic-hydrothermal ore system of Central Kazakhstan. Tectonophysics 328, 69–87.CrossRefGoogle Scholar
Hong, DW, Wang, SG, Xie, XL and Zhang, JS (2000) Genesis of positive ϵNd(t) granitoids in the Great Hinggan Range–Mongolia orogenic belt and growth continental crust. Earth Science Frontiers 7, 441–56 (in Chinese with English abstract).Google Scholar
Hou, ML, Ding, X and Jiang, SY (2004) Lead and sulfur isotope geochemistry of the Hexi Gold deposit in Penglai Eastern Shandong. Acta Geoscientica Sinica 25, 145–50 (in Chinese with English abstract).Google Scholar
Hou, KJ, Li, YH and Tian, YY (2009) In situ U–Pb zircon dating using laser ablation-multi ion counting-ICP–MS. Mineral Deposits 28, 481–92 (in Chinese with English abstract).Google Scholar
Hou, KJ, Li, YH, Zhou, 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
Irber, W (1999) The lanthanide tetrad effect and its correlation with K/Rb, Eu/Eup, Sr/Eu, Y/Ho, and Zr/Hf of evolving peraluminous granite suites. Geochimica et Cosmochimca Acta 63, 489–508.CrossRefGoogle Scholar
Jahn, BM (2004) The Central Asian Orogenic Belt and growth of the continental crust in the Phanerozoic. In Aspects of the Tectonic Evolution of China (eds Malpas, J, Fletcher, CJN, Ali, JR and Aitchison, JC), pp. 73–100. Geological Society of London, Special Publication no. 226. CrossRefGoogle Scholar
Jahn, BM, Capdevila, R, Liu, DY, Vernon, A and Badarch, G (2004) Sources of Phanerozoic granitoids in the transect Bayanhongor-Ulaan Baatar, Mongolia: geochemical and Nd isotopic evidence, and implications for Phanerozoic crustal growth. Journal of Asian Earth Sciences 23, 629–53.CrossRefGoogle Scholar
Jahn, BM, Wu, FY, Capdevila, R, Fourcade, S, Wang, YX and Zhao, ZH (2001) Highly evolved juvenile granites with tetrad REE patterns: the Woduhe and Baerzhe granites from the Great Xing’an (Khingan) Mountains in NE China. Lithos 59, 171–98.CrossRefGoogle Scholar
Jahn, BM, Wu, FY and Chen, B (2000a) Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic. Transactions of the Royal Society of Edinburgh: Earth Sciences 91, 181–93.CrossRefGoogle Scholar
Jahn, BM, Wu, FY and Chen, B (2000b) Massive granitoid generation in Central Asia: Nd isotopic evidence and implication for continental growth in the Phanerozoic. Episodes 23, 82–92.CrossRefGoogle Scholar
Jia, PP, Wei, JH, Gong, QW and Zhao, WL (2011) Analysis of geological background and ore-searching prospect for the copper–molybdenum deposits in the Da Hingan Ling area. Geology and Exploration 47, 151–62 (in Chinese with English abstract).Google 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, SH, Liang, QL, Liu, YF and Liu, Y (2012) Zircon U–Pb ages of magmatic rocks occurring in around the Dajing Cu–Ag–Sn polymetallic deposit of Inner Mongolia constrains to the ore-forming age. Acta Petrologica Sinica 28, 495–513 (in Chinese with English abstract).Google Scholar
Jiang, SH, Nie, FJ, Bai, DM, Liu, YF and Liu, Y (2011a) Geochronology evidence for Indosinian mineralization in Baiyinnuoer Pb–Zn deposit of Inner Mongolia. Mineral Deposits 30, 787–98 (in Chinese with English abstract).Google Scholar
Jiang, SH, Nie, FJ, Liu, YF, Hou, WR, Bai, DM, Liu, Y and Liang, QL (2011b) Geochronology of intrusive rocks occurring in and around the Mengentaolegai Ag-polymetallic deposit, Inner Mongolia. Journal of Jilin University (Earth Sciences Edition) 41, 1755–69 (in Chinese with English abstract).Google Scholar
Jiang, SH, Nie, FJ, Liu, YF and Yun, F (2010) Sulfur and lead isotopic compositions of Bairendaba and Weilasituo silver-polymetallic deposits, Inner Mongolia. Mineral Deposits 28, 101–12 (in Chinese with English abstract).Google Scholar
Jiang, SY, Yang, T, Li, L, Zhao, KD and Ling, HF (2006) Lead and sulfur isotopic compositions of sulfides from the TAG hydrothermal field, Mid-Atlantic Ridge. Acta Petrologica Sinica 22, 2597–602 (in Chinese with English abstract).Google Scholar
Jiang, SH, Zhang, LL, Liu, YF, Liu, CH, Kang, H and Wang, FX (2018) Metallogeny of Xing-Meng Orogenic Belt and some related problems. Mineral Deposits 37, 671–711 (in Chinese with English abstract).Google Scholar
King, PL, Chappell, BW, Allen, CM and White, AJR (2001) Are A-type granites the high-temperature felsic granites? Evidence from fractionated granites of the Wangrah Suite. Journal of the Geological Society of Australia 48, 501–14.Google Scholar
Konecke, BA, Fiege, A, Simon, AC, Parat, F and Stechern, A (2017) Co-variability of S6+, S4+, and S2- in apatite as a function of oxidation state: implications for a new oxybarometer. American Mineralogist 102, 548–57.CrossRefGoogle Scholar
Kovalenko, VI, Yarmolyuk, VV, Kovach, VP, Kotov, AB, Kozakov, IK and Sal’nikova, EB (1996) Sources of Phanerozoic granitoids in Central Asia: Sm–Nd isotope data. Geochemical International 34, 628–40.Google Scholar
Li, JW, Bi, SY, Selby, D, Chen, L, Vasconcelos, P, Thiede, D, Zhou, MF, Zhao, XF, Li, ZK and Qiu, HN (2012) Giant Mesozoic gold provinces related to the destruction of the North China Craton. Earth and Planetary Science Letters 349–350, 26–37.CrossRefGoogle Scholar
Li, X, Chi, G, Zhou, Y, Deng, T and Zha, J (2017) Oxygen fugacity of Yanshanian granites in South China and implications for metallogeny. Ore Geology Reviews 88, 690–701.CrossRefGoogle Scholar
Li, XH, Li, WX and Li, ZX (2007) On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China. China Science Bulletin 52, 984–91 (in Chinese with English abstract).CrossRefGoogle Scholar
Li, ZZ, Qin, KZ, Li, GM, Ishihara, S, Jin, LY, Song, GX and Meng, ZJ (2014a) Formation of the giant Chalukou porphyry Mo deposit in northern Great Xing’an Range, NE China: partial melting of the juvenile lower crust in intra-plate extensional environment. Lithos 202–203, 138–56.CrossRefGoogle Scholar
Li, JF, Wang, KY, Quan, HY, Sun, FY, Zhao, LS and Zhang, XB (2016) Discussion on the magmatic evolution sequence and metallogenic geodynamical setting background Hongling Pb–Zn deposit in the southern Da Xing’an Mountains. Acta Petrologica Sinica 32, 1529–42 (in Chinese with English abstract).Google Scholar
Li, PZ and Yu, JS (1993) Nianzishan miarolitic alkaline granite stock, Heilongjiang—its ages and geological implications. Geochimica 22, 389–98 (in Chinese with English abstract).Google Scholar
Li, Y, Zhou, H, Brouwer, FM, Xiao, W, Wijbrans, JR and Zhong, Z (2014b) Early Paleozoic to Middle Triassic bivergent accretion in the Central Asian Orogenic Belt: insights from zircon U–Pb dating of ductile shear zones in central Inner Mongolia, China. Lithos 205, 84–111.CrossRefGoogle Scholar
Lin, Q, Ge, WC, Wu, FY, Sun, DY and Cao, L (2004) Geochemistry of Mesozoic granites in Da Hinggan Ling ranges. Acta Petrologica Sinica 20, 403–12 (in Chinese with English abstract).Google 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, Han, N, Chen, CL and Kang, H (2017) Isotopic (C–O–S) geochemistry and Re–Os geochronology of the Haobugao Zn–Fe deposit in Inner Mongolia, NE China. Ore Geology Reviews 82, 130–47.CrossRefGoogle Scholar
Liu, YF, Jiang, SH and Zhang, Y (2010) The SHRIMP zircon U–Pb dating and geological features of Bairendaba diorite in the Xilinhaote area, Inner Mongolia, China. Geological Bulletin of China 29, 688–96 (in Chinese with English Abstract).Google Scholar
Liu, W, Pan, XF, Xie, LW and Li, H (2007) Sources of material for the Linxi granitoids, the southern segment of the Da Hinggan Mts.: when and how continental crust grew? Acta Petrologica Sinica 23, 441–60 (in Chinese with English abstract).Google Scholar
Liu, W, Siebel, W, Li, XJ and Pan, XF (2005) Petrogenesis of the Linxi granitoids, northern Inner Mongolia of China: constraints on basaltic underplating. Chemical Geology 219, 5–35.CrossRefGoogle Scholar
Liu, LJ, Zhou, TF, Zhang, DY, Yuan, F, Liu, GX, Zhao, ZC, Sun, JD and White, N (2018) S isotopic geochemistry, zircon and cassiterite U–Pb geochronology of the Haobugao Sn polymetallic deposit, southern Great Xing’an Range, NE China. Ore Geology Reviews 93, 168–80.CrossRefGoogle Scholar
Ludwig, KR (2003). User’s Manual for Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley: Berkeley Geochronology Center Special Publication no. 4.Google Scholar
Mao, JW, Wang, YT, Lehmann, B, Yu, JJ, Du, AD, Mei, YX, Li, YT, Zang, WS, Stein, HJ and Zhou, TF (2006) Molybdenite Re–Os and albite 40Ar/39Ar dating of Cu–Au–Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications. Ore Geology Reviews 29, 307–24.CrossRefGoogle Scholar
Mao, JW, Xie, GQ, Bierlein, F, Qu, WJ, Du, AD, Ye, HS, Pirajno, F, Li, HM, Guo, BJ, Lie, YF and Yang, ZQ (2008) Tectonic implications from Re–Os dating of Mesozoic molybdenum deposits in the East Qinling–Dabie orogenic belt. Geochimica et Cosmochimica Acta 72, 4607–26.CrossRefGoogle Scholar
Mao, JW, Xie, GQ, Pirajno, F, Ye, HS, Wang, YB, Li, YF, Xiang, JF and Zhao, HJ (2010) Late Jurassic–Early Cretaceous granitoid magmatism in East Qinling, central-eastern China: SHRIMP zircon U–Pb ages and tectonic implications. Australian Journal of Earth Sciences 57, 51–78.CrossRefGoogle Scholar
Mao, JW, Xie, GQ, Zhang, ZH, Li, XF, Wang, YT, Zhang, CQ and Li, YF (2005) Mesozoic large-scale metallogenic pulses in North China and corresponding geodynamic settings. Acta Petrologica Sinica 21, 169–88 (in Chinese with English abstract).Google Scholar
Marks, MA, Wenzel, T, Whitehouse, MJ, Loose, M, Zack, T, Barth, M, Barth, M, Worgard, L, Krasz, V, Eby, GN, Stosnach, H and Markl, G (2012) The volatile inventory (F, Cl, Br, S, C) of magmatic apatite: an integrated analytical approach. Chemical Geology 291, 241–55.CrossRefGoogle Scholar
Martin, H (1999) Adakitic magmas: modern analogues of Archaean granitoids. Lithos 46, 411–29.CrossRefGoogle Scholar
Mathez, EA and Webster, JD (2005) Partitioning behavior of chlorine and fluorine in the system apatite–silicate melt–fluid. Geochimica et Cosmochimica Acta 69, 1275–86.CrossRefGoogle Scholar
Meng, QR (2003) What drove late Mesozoic extension of the northern China–Mongolia tract? Tectonophysics 369, 155–74.CrossRefGoogle Scholar
Miles, AJ, Graham, CM, Hawkesworth, CJ, Gillespie, MR, Hinton, RW and Bromiley, GD (2014) Apatite: a new redox proxy for silicic magmas? Geochimica et Cosmochimica Acta 132, 101–19.CrossRefGoogle Scholar
Miller, CF and Mittlefehldt, DW (1982) Depletion of light rare-earth elements in felsic magmas. Geology 10, 129–33.2.0.CO;2>CrossRefGoogle Scholar
Miller, CF and Mittlefehldt, DW (1984) Extreme fractionation in felsic magma chambers: a product of liquid-state diffusion or fractional crystallization? Earth and Planetary Science Letters 68, 151–8.CrossRefGoogle Scholar
Mitchell, R, Chudy, T, McFarlane, CR and Wu, FY (2017) Trace element and isotopic composition of apatite in carbonatites from the Blue River area (British Columbia, Canada) and mineralogy of associated silicate rocks. Lithos 286–287, 75–91.CrossRefGoogle Scholar
Nesbitt, HW and Young, GM (1982) Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature 299, 715–7.CrossRefGoogle Scholar
Nie, FJ, Jiang, SH, Su, XX and Wang, XL (2002) Geological features and origin of gold deposits occurring in the Baotou-Bayan Obo district, south-central Inner Mongolia, People’s Republic of China. Ore Geology Reviews 30, 1–29.Google Scholar
Ouyang, HG, Mao, JW, Santosh, M, Wu, Y, Hou, L and Wang, XF (2014) The Early Cretaceous Weilasituo Zn–Cu–Ag vein deposit in the southern Great Xing’an Range, northeast China: fluid inclusions, H, O, S, Pb isotope geochemistry and genetic implications. Ore Geology Reviews 56, 503–15.CrossRefGoogle Scholar
Ouyang, HG, Mao, JW, Santosh, M, Zhou, J, Zhou, ZH, Wu, Y and Hou, L (2013) Geodynamic setting of Mesozoic magmatism in NE China and surrounding regions: perspectives from spatio-temporal distribution patterns of ore deposits. Journal of Asian Earth Sciences 78, 222–36.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
Pan, LC, Hu, RZ, Wang, XS, Bi, XW, Zhu, JJ and Li, C (2016) Apatite trace element and halogen compositions as petrogenetic–metallogenic indicators: examples from four granite plutons in the Sanjiang region, SW China. Lithos 254, 118–30.CrossRefGoogle Scholar
Piccoli, PM and Candela, PA (1994) Apatite in felsic rocks; a model for the estimation of initial halogen concentrations in the Bishop Tuff (Long Valley) and Tuolumne Intrusive Suite (Sierra Nevada Batholith) magmas. American Journal of Science 294, 92–135.CrossRefGoogle Scholar
Poli, GE and Tommasini, S (1991) Model for the origin and significance of microgranular enclaves in calc-alkaline granitoids. Journal of Petrology 32, 657–66.CrossRefGoogle Scholar
Prowatke, S and Klemme, S (2006) Trace element partitioning between apatite and silicate melts. Geochimica et Cosmochimica Acta 70, 4513–27.CrossRefGoogle Scholar
Qiu, JT, Yu, XQ, Santosh, M, Zhang, DH, Chen, SQ and Li, PJ (2013) Geochronology and magmatic oxygen fugacity of the Tongcun molybdenum deposit, northwest Zhejiang, SE China. Mineralium Deposita 48, 545–56.CrossRefGoogle Scholar
Richards, JP (2003) Tectono-magmatic precursors for porphyry Cu-(MoAu) deposit formation. Economic Geology 98, 1515–33.CrossRefGoogle Scholar
Ruan, BX, Lv, XB, Yang, W, Liu, ST, Yu, YM, Wu, CM and Munir, MAA (2015) Geology, geochemistry and fluid inclusions of the Bianjiadayuan Pb–Zn–Ag deposit, Inner Mongolia, NE China: implications for tectonic setting and metallogeny. Ore Geology Reviews 71, 121–37.CrossRefGoogle Scholar
Rui, ZY, Shi, LD and Fang, R (1994) Deposit Geology of the Non-ferrous Metal Deposits in the Northern Margin of North China and Adjacent Areas. Beijing: Geological Publishing House, 476 pp. (in Chinese with English abstract).Google Scholar
Scott, JA, Humphreys, MC, Mather, TA, Pyle, DM and Stock, MJ (2015) Insights into the behaviour of S, F, and Cl at Santiaguito Volcano, Guatemala, from apatite and glass. Lithos 232, 375–94.CrossRefGoogle Scholar
Sha, LK and Chappell, BW (1999) Apatite chemical composition, determined by electron microprobe and laser-ablation inductively coupled plasma mass spectrometry, as a probe into granite petrogenesis. Geochimica et Cosmochimica Acta 63, 3861–81.CrossRefGoogle Scholar
Shao, JA, Han, QJ, Zhang, LQ and Mu, BL (1999) Cumulate complex xenoliths in the Early Mesozoic eastern Inner Mongolia. China Science Bulletin 44, 1272–9 (in Chinese with English abstract).CrossRefGoogle Scholar
Shao, JA, Liu, FT, Chen, H and Han, QJ (2001) Relationship between Mesozoic magmatism and subduction in Da Hinggan – Yanshan area. Acta Geologica Sinica 75, 56–63 (in Chinese with English abstract).Google Scholar
Shao, JA, Mu, BL, Zhu, HZ and Zhang, LQ (2010) Material source and tectonic settings of the Mesozoic mineralization of the Great Hinggan Range. Acta Petrologica Sinica 26, 649–56 (in Chinese with English abstract).Google Scholar
Sheng, JF and Fu, XZ (1999) Metallogenetic Environment and Geological Characteristics of Copper-Polymetallic Ore Deposits in Middle Part of Da Hinggan Mts. Beijing: Seismological Publishing House (in Chinese).Google Scholar
Shu, QH, Lai, Y, Sun, Y, Wang, C and Meng, S (2013a) Ore genesis and hydrothermal evolution of the Baiyinnuo’er zinc–lead skarn deposit, Northeast China: evidence from isotopes (S, Pb) and fluid inclusions. Economic Geology 108, 835–60.CrossRefGoogle Scholar
Shu, QH, Lai, Y, Wang, C, Xu, JJ and Sun, Y (2013b) Geochronology, geochemistry and Sr–Nd–Hf isotopes of the Haisugou porphyry Mo deposit, northeast China, and their geological significance. Journal of Asian Earth Sciences 79, 777–91.CrossRefGoogle Scholar
Sillitoe, RH (2010) Porphyry copper systems. Economic Geology 105, 3–41.Google Scholar
Sisson, TW, Ratajeski, K and Hankins, WB (2005) Voluminous granitic magmas from common basaltic sources. Contributions to Mineralogy and Petrology 148, 635–61.CrossRefGoogle Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In Magmatism in the Ocean Basins (eds Saunders, AD and Norry, MJ), pp. 313–45. Geological Society of London, Special Publication no. 42. CrossRefGoogle Scholar
Sun, DY, Wu, FY, Li, HM and Lin, Q (2001) Emplacement age of the postorogenic A-type granites in northwestern Lesser Xing’an Ranges, and its relationship to the eastward extension of Suolunshan–Hegenshan–Zhalaite collisional suture zone. China Science Bulletin 46, 427–32 (in Chinese with English abstract).CrossRefGoogle Scholar
Tacker, RC and Stormer, JC (1989) A thermodynamic model for apatite solid solutions, applicable to high-temperature geologic problems. American Mineralogist 74, 877–88.Google Scholar
Taylor, SR and McLennan, SM (1985) The Continental Crust: Its Composition and Evolution. Oxford: Blackwell Scientific Publications, 312 pp.Google Scholar
Tepley, FJ, Davidson, JP, Tilling, RI and Arth, JG (2000) Magma mixing, recharge and eruption histories recorded in plagioclase phenocrysts from El Chichon Volcano, Mexico. Journal of Petrology 41, 1397–411.CrossRefGoogle Scholar
Wang, CY (2015) Lead-zinc polymetallic metallogenic series and prospecting direction of Huanggangliang – Ganzhuermiao metallogenic belt, Inner Mongolia. Ph.D. thesis, Jilin University, Changchun, China. Published thesis.Google Scholar
Wang, XD, Xu, DM, Lv, XB, Wei, W, Mei, W, Fan, XJ and Sun, BK (2018) Origin of the Haobugao skarn Fe-Zn polymetallic deposit, Southern Great Xing’an Range, NE China: geochronological, geochemical, and Sr–Nd–Pb isotopic constraints. Ore Geology Reviews 94, 58–72.CrossRefGoogle Scholar
Wang, Q, Xu, JF, Zhao, ZH, Bao, ZW, Xu, W and Xiong, XL (2004) Cretaceous high potassium intrusive rocks in the Yueshan–Hongzhen area of east China: adakites in an extensional tectonic regime within a continent. Geochemical Journal 38, 417–34.CrossRefGoogle Scholar
Wang, YX and Zhao, ZH (1997) Geochemistry and origin of the Baerzhe REE–Nb–Be–Zr superlarge deposit. Geochimica 26, 24–35 (in Chinese with English abstract).Google 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, BE and Green, HT (1981) Apatite/liquid partition coefficients for the rare earth elements and strontium. Earth and Planetary Science Letters 56, 405–21.CrossRefGoogle Scholar
Watson, BE and Harrison, MT (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, Tappen, CM and Mandeville, CW (2009) Partitioning behavior of chlorine and fluorine in the system apatite–melt–fluid. II: felsic silicate systems at 200 MPa. Geochimica et Cosmochimica Acta 73, 559–81.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
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
Windley, BF, Alexeiev, D, Xiao, WJ, Kröner, A and Badarch, G (2007) Tectonic models for accretion of the Central Asian Orogenic Belt. Journal of the Geological Society, London 164, 31–47.CrossRefGoogle Scholar
Wu, FY, Jahn, BM, Wilde, SA, Lo, CH, Yui, TF, Lin, Q, Ge, WC and Sun, DY (2003) Highly fractionated I-type granites in NE China (II): isotopic geochemistry and implications for crustal growth in the Phanerozoic. Lithos 67, 191–204.CrossRefGoogle Scholar
Wu, FY, Jahn, BM, Wilde, SA and Sun, DY (2000) Phanerozoic crustal growth: U–Pb and Sr–Nd isotopic evidence from the granites in northeastern China. Tectonophysics 328, 89–113.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, Li, HM, Jahn, BM and Wilde, SA (2002) A-type granites in northeastern China: age and geochemical constraints on their petrogenesis. Chemical Geology 187, 143–73.CrossRefGoogle Scholar
Wu, FY, Sun, DY, Li, HM and Wang, XL (2001) The nature of basement beneath the Songliao Basin in NE China: geochemical and isotopic constraints. Physics and Chemistry of the Earth, Part A 26, 793–803.CrossRefGoogle Scholar
Wu, FY, Sun, DY and Lin, Q (1999) Petrogenesis of the Phanerozoic granites and crustal growth in Northeast China. Acta Petrologica Sinica 15, 181–9 (in Chinese with English abstract).Google Scholar
Wu, HY, Zhang, LC, Wan, B, Chen, ZG, Xiang, P, Pirajno, F, Du, AD, Qu, WJ and Wu, HY (2011a) Re–Os and 40Ar/39Ar ages of the Jiguanshan porphyry Mo deposit, Xilamulun metallogenic belt, NE China, constraints on mineralization events. Mineralium Deposita 46, 171–85.CrossRefGoogle Scholar
Wu, HY, Zhang, LC, Wan, B, Chen, ZG, Zhang, XJ and Xiang, P (2011b) Geochronological and geochemical constraints on Aolunhua porphyry Mo–Cu deposit, northeast China, and its tectonic significance. Ore Geology Reviews 43, 78–91.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Huang, BC, Han, CM, Yuan, C, Chen, HL, Sun, M, Sun, S and Li, JL (2009) End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia. International Journal of Earth Sciences 98, 1189–217.CrossRefGoogle Scholar
Xiao, CD, Zhang, ZL and Zhao, LQ (2004) Nd, Sr and Pb isotope geochemistry of Yanshanian granitoids in eastern Inner Mongolia and their origins. Geology in China 31, 57–63 (in Chinese with English abstract).Google Scholar
Xie, F, Tang, J, Chen, Y and Lang, X (2018) Apatite and zircon geochemistry of Jurassic porphyries in the Xiongcun district, southern Gangdese porphyry copper belt: implications for petrogenesis and mineralization. Ore Geology Reviews 96, 98–114.CrossRefGoogle Scholar
Xu, B, Charvet, J, Chen, Y, Zhao, P and Shi, G (2012) 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 regimes. Journal of Asian Earth Sciences 74, 167–93.CrossRefGoogle Scholar
Zartman, RE and Doe, BR (1981) Plumbotectonics—the model. Tectonophysics 75, 135–62.CrossRefGoogle Scholar
Zeng, QD, Liu, JM, Chu, SX, Wang, YB, Sun, Y, Duan, XX, Zhou, LL and Qu, WJ (2013) Re–Os and U–Pb geochronology of the Duobaoshan porphyry Cu–Mo–(Au) deposit, northeast China, and its geological significance. Journal of Asian Earth Sciences 79, 895–909.CrossRefGoogle Scholar
Zeng, QD, Liu, JM, Yu, CM, Ye, J and Liu, HT (2011) Metal deposits in the Da Hinggan Mountains, NE China styles, characteristics, and exploration potential. International Geology Review 53, 846–78.CrossRefGoogle Scholar
Zeng, QD, Liu, JM and Zhang, ZL (2010) Re–Os geochronology of porphyry molybdenum deposit in south segment of Da Hinggan Mountains, northeast China. Journal of Earth Science 21, 392–401.CrossRefGoogle Scholar
Zhai, DG, Liu, JJ, Wang, JP, Yang, YQ, Zhang, HY, Wang, XL, Zhang, QB, Wang, GW and Liu, ZJ (2014a) Zircon U–Pb and molybdenite Re–Os geochronology, and whole-rock geochemistry of the Hashitu molybdenum deposit and host granitoids, Inner Mongolia, NE China. Journal of Asian Earth Sciences 79, 144–60.CrossRefGoogle Scholar
Zhai, DG, Liu, JJ, Wang, JP, Yao, MJ, Wu, SH, Fu, C, Liu, ZJ, Wang, SG and Li, YX (2013) Fluid evolution of the Jiawula Ag–Pb–Zn deposit, Inner Mongolia: mineralogical, fluid inclusion, and stable isotopic evidence. International Geology Review 55, 204–24.CrossRefGoogle Scholar
Zhai, DG, Liu, JJ and Zhang, HY (2014b) S–Pb isotopic geochemistry, U–Pb and Re–Os geochronology of the Huanggangliang Fe–Sn deposit, Inner Mongolia, NE China. Ore Geology Reviews 59, 109–22.CrossRefGoogle Scholar
Zhang, D, Ai, X and Bao, X (1994) Nonferrous metallic deposits in Huanggang Ganzhuermiao Mesozoic reworking region. In Geology and Nonferrous Metallic Deposits in the Northern Margin of the North China Block and Its Adjacent Area (ed. Rui, Z), pp. 314–63. Beijing: Geological Publishing House.Google Scholar
Zhang, JH, Gao, S, Ge, WC, Wu, FY, Yang, JH, Wilde, SA and Li, M (2010a) Geochronology of the Mesozoic volcanic rocks in the Great Xing’an Range, northeastern China: implications for subduction-induced delamination. Chemical Geology 276, 144–65.CrossRefGoogle Scholar
Zhang, JH, Ge, WC, Wu, FY, Wilde, SA, Yang, JH and Liu, XM (2008a) Large-scale Early Cretaceous volcanic events in the northern Great Xing’an Range, northeastern China. Lithos 102, 138–57.CrossRefGoogle Scholar
Zhang, C, Sun, W, Wang, J, Zhang, L, Sun, S and Wu, K (2017) Oxygen fugacity and porphyry mineralization: a zircon perspective of Dexing porphyry Cu deposit, China. Geochimica et Cosmochimica Acta 206, 343–63.CrossRefGoogle Scholar
Zhang, M, Zhai, YS, Shen, CL, Liu, YH, Yang, SS, Zhai, DG, Yao, MJ, Wang, JP, Wang, SG, Gao, ZX and Zhang, L (2011) Metallogenic system of copper polymetallic deposits in the middle-southern part of Da Hinggan Mountains, China. Geoscience 25, 819–31.Google Scholar
Zhang, XJ, Zhang, LC, Jin, XD, Wu, HY, Xiang, P and Chen, ZG (2010b) U–Pb ages, geochemical characteristics and their implications of Banlashan molybdenum deposit. Acta Petrologica Sinica 26, 1411–22.Google Scholar
Zhang, L, Zhou, X, Ying, J, Wang, F, Guo, F, Wan, B and Chen, Z (2008b) Geochemistry and Sr–Nd–Pb–Hf isotopes of Early Cretaceous basalts from the Great Xinggan Range, NE China: implications for their origin and mantle source characteristics. Chemical Geology 256, 12–23.CrossRefGoogle Scholar
Zhao, YM and Zhang, DQ (1997) Metallogeny and Prospective Evaluation of Copper Polymetallic Deposits in the Da Hinggan Mountains and Surrounding Regions. Beijing: Seismic Publisher (in Chinese).Google Scholar
Zhong, SH, Feng, CY, Seltmann, R, Li, DX and Dai, ZH (2018) Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite). Mineralium Deposita 53, 855–70.CrossRefGoogle Scholar
Zhou, Y, Ge, WC and Wang, QH (2011) Petrogenesis of Mesozoic granite in Wulanhaote region, central Da Hinggan Mountains: constrains from geochemistry and Sr–Nd–Hf isotope. Acta Petrologica et Mineralogica 30, 901–23 (in Chinese with English abstract).Google Scholar
Zhou, ZH, Lü, LS, Yang, YJ and Li, T (2010) Petrogenesis of the Early Cretaceous A-type granite in the Huanggang Sn–Fe deposit, Inner Mongolia: constraints from zircon U–Pb dating and geochemistry. Acta Petrologica Sinica 26, 3521–37 (in Chinese with English abstract).Google Scholar
Zhou, ZH, Mao, JW and Lyckberg, P (2012) Geochronology and isotopic geochemistry of the A-type granites from the Huanggang Sn–Fe deposit, southern Great Hinggan Range, NE China: implication for their origin and tectonic setting. Journal of Asian Earth Sciences 49, 272–86.CrossRefGoogle Scholar
Zhu, RX, Chen, L, Wu, FY and Liu, JL (2011) Timing, scale and mechanism of the destruction of the North China Craton. Science China Earth Sciences 54, 789–97 (in Chinese with English abstract).CrossRefGoogle Scholar
Zhu, RZ, Lai, SC, Qin, JF and Zhao, SW (2015) Early-Cretaceous highly fractionated I-type granites from the northern Tengchong block, western Yunnan, SW China: petrogenesis and tectonic implications. Journal of Asian Earth Sciences 100, 145–63.CrossRefGoogle Scholar
Zhu, XQ, Zhang, Q, He, YL, Zhu, CH and Huang, Y (2006) Hydrothermal source rocks of the Meng’entaolegai Ag–Pb–Zn deposit in the granite batholith, Inner Mongolia, China: constrained by isotopic geochemistry. Geochemical Journal 40, 265–75.CrossRefGoogle Scholar
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