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The granite porphyry hidden in the Shuangjianzishan deposit, southern Great Xing’an Range, NE China: geochronology, isotope geochemistry and tectonic implications

Published online by Cambridge University Press:  08 October 2020

Wei Wei Open the ORCID record for Wei Wei [Opens in a new window] ,
Xin-Biao Lv  and
Xiang-Dong Wang
Wei Wei*
Affiliation:
Institute of Geological Survey, China University of Geosciences, Wuhan430074, China
Xin-Biao Lv*
Affiliation:
Institute of Geological Survey, China University of Geosciences, Wuhan430074, China
Xiang-Dong Wang
Affiliation:
Wuhan Center of Geological Survey (CGS), Wuhan430205, China
*
Author for correspondence: Wei Wei, Emails: [email protected]; [email protected]
Author for correspondence: Wei Wei, Emails: [email protected]; [email protected]
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Abstract

The Shuangjianzishan vein-type Ag-Pb-Zn deposit in the southern Great Xing’an Range (GXR), NE China, is hosted in the slate of the Lower Permian Dashizhai Formation intruded by granite porphyry. In this paper, U–Pb zircon ages and bulk-rock and isotope (Sr, Nd, Pb and Hf) compositions are reported to investigate the derivation, evolution and geodynamic setting of this granite porphyry. It is closely associated with Pb-Zn-Ag mineralization in the southern GXR and contains important geological information relating to regional tectonic evolution. Laser ablation – inductively coupled plasma – mass spectrometry (LA-ICP-MS) zircon U–Pb dating yields an emplacement age of 131 ± 1 Ma for the granite porphyry. Bulk-rock analyses show that the Shuangjianzishan granite porphyry is characterized by high Si, Na and K contents but low Mg and Fe contents, and that the enrichment of Zr, Y and Ga suggests an A-type granite affinity. Most of the studied samples have relatively low 87Sr/86Sr values (0.70549–0.70558), with positive ϵNd(t) (0.71–0.88) and ϵHf(t) (4.9–6.9) values. The Sr–Nd isotope modelling results, in combination with the young TDM2 ages of Nd and Hf (850–864 and 668–778 Ma, respectively), reveal that the Shuangjianzishan granite porphyry may be derived from the melting of mantle-derived juvenile component, with minor lower crustal components; this finding is also supported by Pb isotopic compositions. Considering the widespread presence of granitoids with coeval volcanic rocks and regional geology data, we propose that the Shuangjianzishan granite porphyry formed in a post-orogenic extensional environment related to the upwelling of asthenospheric mantle following the closure of the Mongol–Okhotsk Ocean.

Keywords

granite porphyrychronologyGreat Xing’an RangeShuangjianzishanNE China
Type
Original Article
Information
Geological Magazine , Volume 158 , Issue 6 , June 2021 , pp. 995 - 1009
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

Amelin, Y, Lee, DC and Halliday, AN (2000) Early-Middle Archean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains. Geochimica et Cosmochimica Acta 64, 4205–25.CrossRefGoogle 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 80, 155–77.CrossRefGoogle Scholar
Baxter, S and Feely, M (2002) Magma mixing and mingling textures in granitoids: examples from the Galway Granite, Connemara, Ireland. Mineralogy and Petrology 76, 63–74.CrossRefGoogle Scholar
Bonin, B (1990) From orogenic to anorogenic settings: evolution of granitoid suites after a major orogenesis. Geological Journal 25, 261–70.CrossRefGoogle Scholar
Chappell, BW (1984) Source rocks of I- and S-type granites in the Lachlan Fold Belt, southeastern Australia. Philosophical Transactions of the Royal Society of London A 310, 693–707.Google Scholar
Chappell, BW (1999) Aluminium saturation in I- and S-type granites and the characterization of fractionated hapogranites. Lithos 46, 535–51.CrossRefGoogle Scholar
Chappell, BW, Bryant, CJ and Wyborn, D (2012) Peraluminous I-type granites. Lithos 153, 142–53.CrossRefGoogle Scholar
Chappell, BW and White, AJR (1974) Two contrasting granite types. Pacific Geology 8, 173–74.Google Scholar
Chappell, BW and White, AJR (1992) I- and S-type granites in the Lachlan Fold Belt. Transactions of the Royal Society of Edinburgh: Earth Sciences 83, 1–26.CrossRefGoogle Scholar
Chen, H, Xia, QK, Ingrin, J, Deloule, E and Bi, Y (2017) Heterogeneous source components of intraplate basalts from NE China induced by the ongoing Pacific slab subduction. Earth & Planetary Science Letters 459, 208–20.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
Cogné, JP, Kravchinsky, VA, Halim, N and Hankard, F (2005) Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk Ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baikal area (SE Siberia). Geophysical Journal International 63, 813–32.CrossRefGoogle Scholar
Collins, WJ, Beams, SD, White, AJR and Chappell, BW (1982) Nature and origin A-type granites with particular reference to Southeastern Australia. Contributions to Mineralogy and Petrology 80, 189–200.CrossRefGoogle Scholar
Cui, M (2015) The geochemical characteristics and diagenesis of ore-forming diorite-porphyrite from Shuangjianzishan Ag polymetallic deposit in Inner Mongolia. M.Sc. thesis, Mineral Deposit and Mineral Deposit Geochemistry, China University of Geosciences (Beijing). Published thesis.Google Scholar
Dong, Y, Ge, WC, Yang, H, Zhao, GH, Wang, QH, Zhang, YL and Su, L (2014) Geochronology and geochemistry of Early Cretaceous volcanic rocks from the Baiyingaolao Formation in the central Great Xing’an Range, NE China, and its tectonic implications. Lithos 205, 168–84.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
Fan, WM, Guo, F, Wang, YJ and Lin, G (2003) Late Mesozoic calc-alkaline volcanism of post-orogenic extension in the northern DaHinggan Mountains, Northeastern China. Journal of Volcanology and Geothermal Research 121, 115–35.CrossRefGoogle Scholar
Fritzell, EH, Bull, AL and Shephard, GE (2016) Closure of the Mongol-Okhotsk Ocean: insights from seismic tomography and numerical modelling. Earth & Planetary Science Letters 445, 1–12.CrossRefGoogle Scholar
Gu, YC, Chen, RY, Jia, B and Ju, N (2017) Zircon U-Pb dating and geochemistry of the granite porphyry from the Shuangjianzishan silver polymetallic deposit in Inner Mongolia and tectonic implication. Geology and Exploration 53, 495–507 (in Chinese).Google Scholar
Harris, NBW, 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
Hineab, R, Williams, IS, Chappelle, BW and White, AJR (1978) Contrasts between I- and S-type granitoids of the Kosciusko Batholith. Journal of the Geological Society of Australia 25, 219–34.Google Scholar
Hu, Z, Liu, Y, Gao, S, Liu, WG, Zhang, W, Tong, XR, Lin, L, Zong, KQ, Li, M, Chen, HH, Zhou, L and Yang, L (2012) Improved in situ Hf isotope ratio analysis of zircon using newly designed X skimmer cone and jet sample cone in combination with the addition of nitrogen by laser ablation multiple collector ICP-MS. Journal of Analytical Atomic Spectrometry 27, 1391–99.CrossRefGoogle Scholar
Jahn, BM, Wu, FY, Capdeviala, 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
Jiang, BB, Zhu, XY, Huang, XK, Xu, Q and Zhang, ZQ (2017) Isotopic characteristics of sulfur and lead and metallogenic mechanism of Shuangjianzishan silver polymetallic deposit in Inner Mongolia. Mineral Exploration 8, 1010–19 (in Chinese).Google Scholar
Jiang, SH, Nie, FJ, Bai, DM, Liu, YF and Liu, Y (2011) 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
Kelty, TK, Yin, A, Dash, B, Gehrels, GE and Ribeiro, AE (2008) Detrital-zircon geochronology of Paleozoic sedimentary rocks in the Hangay-Hentey basin, north-central Mongolia: implications for the tectonic evolution of the Mongol-Okhotsk Ocean in central Asia. Tectonophysics 451, 290–311.CrossRefGoogle Scholar
Koschek, G (1993) Origin and significance of the SEM cathodoluminescence from zircon. Journal of Microscopy 171, 223–32.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
Kuang, YS, Zheng, GR, Lu, MJ, Liu, YL, Zhang, SJ, Li, Y and Cheng, WJ (2014) Basic characteristics of Shuangjianzishan sliver polymetallic deposit in Chifeng City, Inner Mongolia. Mineral Deposits 33, 847–56 (in Chinese).Google Scholar
Larson, RL, Pitman, WC, Golovchenko, X, Cande, SC, Dewey, JF, Haxby, WF and La Brecque, JL (1985) The Bedrock Geology of the World. New York: WH Freeman and Company. Google Scholar
Li, JW, Zhao, XF, Zhou, MF, Vasconcelos, P, Ma, CQ, Deng, XD, Souza, ZS, Zhao, YX and Wu, G (2008) Origin of the Tongshankou porphyry-skarn Cu-Mo deposit, eastern Yangtze craton, Eastern China: geochronological, geochemical, and Sr-Nd-Hf isotopic constraints. Mineralium Deposita 43, 315–36.CrossRefGoogle Scholar
Li, JY, Guo, F, Li, CW, Li, HX and Zhao, L (2014) Neodymium isotopic variations of Late Paleozoic to Mesozoic I- and A-type granitoids in NE China: implications for tectonic evolution. Acta Petrologica Sinica 30, 1995–2008 (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, 389–97 (in Chinese with English abstract).Google Scholar
Li, XH, Liu, DY, Sun, M, Li, WX, Liang, XR and Liu, Y (2004) Precise Sm-Nd and U-Pb isotopic dating of the super-giant Shizhuyuan polymetallic deposit and its host granite, Southeast China. Geological Magazine 141, 225–231.CrossRefGoogle Scholar
Li, XH and McCulloch, MT (1998) Geochemical characteristics of Cretaceous mafic dikes from Northern Guangdong, SE China: age, origin and tectonic significance. In Mantle Dynamics and Plate Interactions in East Asia (eds Flower, MFJ, Chung, SL, Lo, CH and Lee, YT), pp. 405–19. Washington: American Geophysical Union 27, 405–19.CrossRefGoogle Scholar
Liu, CH, Bagas, L and Wang, F (2016) Isotopic analysis of the super-large Shuangjianzishan Pb–Zn–Ag deposit in Inner Mongolia, China: constraints on magmatism, metallogenesis, and tectonic setting. Ore Geology Reviews 75, 252–267.CrossRefGoogle Scholar
Liu, HZ (2017) Discussion on Metallogenic characteristics and Genesis of Weilasituo Sn Polymetal Deposit in Inner Mongolia. Ph.D. thesis, China University of Geosciences (Beijing). Published thesis.Google Scholar
Liu, K, Zhang, JJ, Wilde, SA, Zhou, JB, Wang, M, Ge, MH, Wang, JM and Ling, YY (2017) Initial subduction of the Paleo-Pacific oceanic plate in NE China: constraints from whole-rock geochemistry and zircon U-Pb and Lu-Hf isotopes of the Khanka Lake granitoids. Lithos 274, 254–70.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 of mantle xenoliths. Journal of Petrology 51, 537–71.CrossRefGoogle Scholar
Liu, YS, Hu, ZC, Gao, S, Gunther, D, Xu, J, Gao, CG and Chen, HH (2008) In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology 257, 34–43.CrossRefGoogle Scholar
Liu, Y, Jiang, SH, Leon, B, 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(3), 411–34.CrossRefGoogle Scholar
Ludwig, KR (2003) User’s Manual for Isoplot 3.0-a Geochronological Toolkit for Microsoft Excel . Berkeley Geochronology Center, Special Publication 4, 1–70.Google Scholar
Ma, XH, Cao, R, Zhou, ZH and Zhu, WP (2015) Early Cretaceous high-Mg diorites in the Yanji area, northeastern China: petrogenesis and tectonic implications. Journal of Asian Earth Sciences 97, 393–405.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
Mei, W, Lv, XB, Cao, XF, Liu, Z, Zhao, Y, Ai, ZL, Tang, RK and Munir, MA (2014) Ore genesis and hydrothermal evolution of the Huanggang skarn iron-tin pollymetallic deposit, southern Great Xing’an Range: evidence from fluid inclusions and isotope analyses. Ore Geology Reviews 64, 239–52.CrossRefGoogle Scholar
Mei, W, Lv, 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
Meng, QR (2003) What drove late Mesozoic extension of the northern China-Mongolia tract? Tectonophysics 369, 155–74.CrossRefGoogle Scholar
Metelkin, DV, Vemikovsky, VA and Kazansky, AY (2010) Late Mesozoic tectonics of central Asia based on paleomagnetic evidence. Gondwana Research 18, 400–19.CrossRefGoogle Scholar
Miao, LC, Liu, DY, Zhang, FQ, Fan, WM, Shi, YR and Xie, HQ (2007) Zircon SHRIMP U–Pb ages of the “Xinghuadukou Group” in Hanjiayuanzi and Xinlin areas and the “Zhalantun Group” in Inner Mongolia, Da Hinggan Mountains. Chinese Science Bulletin 52, 1112–24.CrossRefGoogle Scholar
Nedelec, A, Stephens, WE and Fallick, AE (1995) The Panafrican stratoid granites of Madagascar: alkaline magmatism in a post-collisional extensional setting. Journal of Petrology 36, 1367–91.CrossRefGoogle Scholar
Ouyang, HG, Li, RH and Zhou, ZH (2016) The Jurassic mineralization of the Shuangjianzishan Ag-polymetallic deposit and its significance in prospecting: evidence from geochronology. Acta Geologica Sinica 90, 1835–45 (in Chinese).Google Scholar
Ouyang, HG, Mao, JW and Santosh, M (2013) Anatomy of a large Ag-Pb-Zn deposit in the Great Xing’an Range, northeast China: metallogeny associated with Early Cretaceous magmatism. International Geology Review 55, 411–29.CrossRefGoogle 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 Review 56, 503–15.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, XF, Guo, LJ, Wang, S, Xue, HM, Hou, ZQ, Tong, Y and Li, ZM (2009) Laser microprobe Ar-Ar dating of biotite from the Weilasituo Cu-Zn polymetallic deposit in Inner Mongolia. Acta Petrologicaet Mineralogica 28, 475–79 (in Chinese with English abstract).Google Scholar
Pearce, JA (1996) Sources and settings of granitic rocks. Episodes 19, 120–25.CrossRefGoogle Scholar
Peccerillo, A and Taylor, SR (1976) Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey. Contributions to Mineralogy and Petrology 58, 63–81.CrossRefGoogle Scholar
Pei, F, Xu, W, Yang, D, Zhao, Q, Liu, X and Hu, Z (2007) Zircon U–Pb geochronology of basement metamorphic rocks in the Songliao Basin. Chinese Science Bulletin 52, 942–48.CrossRefGoogle Scholar
Pupin, JP (1980) Zircon and granite petrology. Contributions to Mineralogy and Petrology 73, 207–20.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 Monglia, NE China: implications for tectonic setting and metallogeny. Ore Geology Reviews 71, 121–37.CrossRefGoogle Scholar
Shu, QH, Lai, Y, Sun, Y, Wang, C and Meng, S (2013) 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
Sui, ZM, Ge, WC, Wu, FY, Zhang, JH, Xu, XC and Chang, RY (2007) Zircon U-Pb ages, geochemistry and its petrogenesis of Jurassic granites in northeastern part of the Da Hinggan Mts. Acta Petrologica Sinica 23, 461–80 (in Chinese with English abstract).Google Scholar
Sun, DY, Wu, FY, Li, HM and Lin, Q (2000) 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. Chinese Science Bulletin 45, 2217–22 (in Chinese with English abstract).Google Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalt: implication for mantle composition and processes. In Magmatism in the Ocean Basin (eds Saunders, AD and Morry, MJ), pp. 528–48. Geological Society of London, Special Publication no. 42.Google Scholar
Sylvester, PJ (1989) Post-collisional alkaline granites. Journal of Geology 97, 261–80.CrossRefGoogle Scholar
Tang, J, Xu, WL, Wang, F, Zhao, S and Wang, W (2016) Early Mesozoic southward subduction history of the Mongol-Okhotsk oceanic plate: evidence from geochronology and geochemistry of Early Mesozoic intrusive rocks in the Erguna Massif, NE China. Gondwana Research 31, 218–40.CrossRefGoogle Scholar
Tang, ZY, Sun, DY and Mao, AQ (2020) Geochemistry of Late Mesozoic volcanic rocks in the central Great Xing’an Range, NE China: petrogenesis and crustal growth in comparison with adjacent areas. International Geology Review 62(1), doi: 10.1080/00206814.2019.1590867.CrossRefGoogle Scholar
Tian, DX, Ge, WC, Yang, H, Zhao, GC and Zhang, YL (2014) Lower Cretaceous alkali feldspar granites in the central part of the Great Xing’an Range, northeastern China: chronology, geochemistry and tectonic implications. Geological Magazine 152, 383–99.CrossRefGoogle Scholar
Wang, FX, Sun, HJ, Pei, RF, Liu, YF, Liu, CH and Jiang, SH (2016a) The geologic features and genesis of Shuangjianzishan Silver-Polymetallic deposit, Balinzuo Qi, Inner Mongolia. Geological Review 62, 1242–56 (in Chinese).Google Scholar
Wang, F, Zhou, XH, Zhang, LC, Ying, JF, Zhang, YT, Wu, FY and Zhu, RX (2006a) 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
Wang, PJ, Chen, FK, Chen, SM, Wolfgang, S and Muharrem, S (2006b) Geochemical and Nd-Sr-Pb isotopic composition of Mesozoic volcanic rocks in the Songliao basin, NE China. Geochemical Journal 40, 149–59.CrossRefGoogle 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, ZJ, Xu, WL, Pei, FP, Wang, ZW, Li, Y and Cao, HH (2015) Geochronology and geochemistry of middle Permian-Middle Triassic intrusive rocks from central-eastern Jilin Province, NE China: constraints on the tectonic evolution of the eastern segment of the Paleo-Asian Ocean. Lithos 238, 13–25.CrossRefGoogle Scholar
Wang, ZW, Pei, FP, Xu, WL, Cao, HH, Wang, ZJ and Zhang, Y (2016b) Tectonic evolution of the eastern Central Asian Orogenic Belt: evidence from zircon U-Pb-Hf isotopes and geochemistry of early Paleozoic rocks in Yanbian region, NE China. Gondwana Research 38, 334–50.CrossRefGoogle Scholar
Wei, GJ, Liang, XR, Li, XH and Liu, Y (2002) Precise measurement of Sr isotopic composition of liquid and solid base using (LP) MC-ICP-MS. Geochimica 31, 295–99 (in Chinese with English abstract).Google 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
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, J, Wilde, SA, Zhang, XO and Yang, JH (2005a) 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 and Sun, DY (1999) The Mesozoic magmatism and lithospheric thinning in Eastern China. Journal of Changchun Science and Technology University 29, 313–8 (in Chinese with English abstract).Google 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
Wu, FY, Sun, DY, Li, HM, Jahn, BM and Wilde, S (2002) A-type granites in northeastern China: age and geochemical constraints on their petrogenesis. Chemical Geology 187, 143–73.CrossRefGoogle Scholar
Wu, FY, Yang, JH, Lo, CH, Wilde, SA, Sun, DY and Jahn, BM (2007) The Heilongjiang Group a Jurassic accretionary complex in the Jiamusi Massif at the western Pacific margin of northeastern China. Island Arc 16, 156–72.CrossRefGoogle Scholar
Wu, FY, Yang, JH, Wilde, SA and Zhang, XO (2005b) Geochronology, petrogenesis and tectonic implications of the Jurassic granites in the Liaodong Peninsula, NE China. Chemical Geology 221, 127–56.CrossRefGoogle Scholar
Wu, GB, Liu, JM, Zeng, QD, Liu, MT, Sun, HS, Yin, ZW and Yin, X (2014) Occurrences of silver in the Shuangjianzishan Pb-Zn-Ag deposit and its implications for mineral processing. Earth Science Frontier 21, 105–15.Google Scholar
Wu, GB, Liu, JM, Zeng, QD, Sun, HS and Liu, MT (2013) Metallogenic age of the Shuangjianzishan Pb-Zn-Ag deposit in Geat Xing’an Range, Inner Mongolia. Acta Mineralogica Sinica 33, Supplement(619), 619 (in Chinese).Google Scholar
Wu, G, Sun, FY, Zhao, CS, Li, ZT, Zhao, AL, Pang, QB and Li, GY (2005c) Discovery of the Early Paleozoic post-collisional granites in northern margin of the Erguna massif and its geological significance. Chinese Science Bulletin 50, 2733–43.CrossRefGoogle Scholar
Xu, JF and Castillo, PR (2004) Geochemical and Nd-Pb isotopic characteristics of the Tethyan asthenosphere: implications for the origin of the Indian Ocean mantle domain. Tectonophysics 393, 9–27.CrossRefGoogle Scholar
Xu, JF, Castillo, PR, Li, XH, Yu, XY, Zhang, BR and Han, YW (2002) MORB-type rocks from the Paleo-Tethyan Mian-Lueyang northern ophiolite in the Qinling Mountains, central China: implications for the source of the low 206Pb/204Pb and high 143Nd/144 Nd mantle component in the Indian Ocean. Earth & Planetary Science Letters 198, 323–37.CrossRefGoogle Scholar
Yang, JH, Wu, FY, Shao, JA, Wilde, SA, Xie, LW and Liu, XM (2006) Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt, North China. Earth and Planetary Science Letters 246, 336–52.CrossRefGoogle Scholar
Yang, WB, Niu, HC, Shan, Q, Sun, WD, Zhang, H, Li, NB, Jiang, YH and Yu, XY (2013) Geochemistry of magmatic and hydrothermal zircon from the highly evolved Baerzhe alkaline granite: implications for Zr-REE-Nb mineralization. Mineralium Deposita 49, 451–70.CrossRefGoogle Scholar
Yang, Y, Gao, FH, Chen, JS, Zhou, Y, Zhang, J, Jin, X and Zhang, YL (2012) Zircon U-Pb ages of Mesozoic volcanic rocks in Chifeng area. Journal of Jilin University 42, 257–68 (in Chinese with English abstract).Google Scholar
Ying, JF, Zhou, XH, Zhang, LC and Wang, F (2010) Geochronological framework of Mesozoic volcanic rocks in the Great Xing’an Range, NE China, and their geodynamic implications. Journal of Asian Earth Sciences 39, 786–93.CrossRefGoogle Scholar
Zartman, RE and Doe, BR (1981) Plumbotectonics – the model. Tectonophysics 75, 135–62.CrossRefGoogle Scholar
Zeng, QD, Qin, KZ, Liu, JM, Li, GM, Zhai, MG, Chu, SX and Guo, YP (2015) Porphyry molybdenum deposits in the Tianshan-Xingmeng orogenic belt, northern China. International Journal of Earth Sciences 104, 991–1023.CrossRefGoogle Scholar
Zhai, DG, Anthony, EW-J, Liu, JJ, David, S, Panagiotis, CV, Stylianos, T, Li, K, Li, PL and Sun, HJ (2020) The Genesis of the giant Shuangjianzishan epithermal Ag-Pb-Zn deposit, Inner Mongolia, Northeastern China. Economic Geology 115, 101–28.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).Google Scholar
Zhai, DG, Liu, JJ, Zhang, HY, Yao, MJ, Wang, JP and Yang, YQ (2014) S-Pb isotopic geochemistry, U-Pb and Re-Os geochronology of the Huanggangliang Fe–Sn deposit, Inner Mongolia, NE China. Ore Geology Reviews 59, 109–122.CrossRefGoogle Scholar
Zhang, HF, Parrish, R, Zhang, L, Xu, WC, Yuan, HL, Gao, S and Crowley, QG (2007) A-type granite and adakitic magmatism association in Songpan–Garze fold belt, eastern Tibetan Plateau: implication for lithospheric delamination. Lithos 97, 323–35.CrossRefGoogle Scholar
Zhang, JH, Gao, S, Ge, WC, Wu, FY, Yang, JH, Wilde, SA and Li, M (2010) 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 (2008) Large-scale Early Cretaceous volcanic events in the northern Great Xing’an Range, Northeastern China. Lithos 102, 138–57 (in Chinese with English abstract).CrossRefGoogle Scholar
Zhang, ZQ (2018) Geological and geochemical characteristics and metallogenetic mechanism of the Shuangjianzishan Ag-polymetallic deposit, Inner Mongolia. M.Sc. thesis, Geology and Geochemistry of Ore Deposit, China University of Geosciences (Beijing). Published thesis.CrossRefGoogle Scholar
Zorin, YA (1999) Geodynamics of the western part of the Mongolia-Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia. Tectonophysics 306, 33–56.CrossRefGoogle Scholar