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Geochronology, geochemistry and tectonic implications of late Carboniferous Daheyan intrusions from the Bogda Mountains, eastern Tianshan

Published online by Cambridge University Press:  29 July 2019

Xuebing Zhang Open the ORCID record for Xuebing Zhang [Opens in a new window] ,
Fengmei Chai ,
Chuan Chen ,
Hongyan Quan  and
Xiaoping Gong
Xuebing Zhang
Affiliation:
College of Geology and Mining Engineering, Xinjiang University, Urumqi 830047, China
Fengmei Chai
Affiliation:
College of Geology and Mining Engineering, Xinjiang University, Urumqi 830047, China
Chuan Chen
Affiliation:
College of Geology and Mining Engineering, Xinjiang University, Urumqi 830047, China
Hongyan Quan
Affiliation:
School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, New South Wales 2052, Australia
Xiaoping Gong*
Affiliation:
College of Geology and Mining Engineering, Xinjiang University, Urumqi 830047, China
*
Author for correspondence: Xiaoping Gong, Email: 504642842@qq.com
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Abstract

The Daheyan region, situated in the SW of the Bogda Mountains in eastern Tianshan, is important for understanding the accretionary history of the Central Asian Orogenic Belt. We investigated Carboniferous intrusions from the Daheyan area, SW Bogda Mountains, obtaining new zircon U–Pb ages, whole-rock geochemical data and Hf isotope data for these intrusions. Zircon U–Pb dating indicates that syenogranite, diorite, granodiorite and monzonite of the Daheyan intrusions were all formed during late Carboniferous (311–303 Ma) magmatism. The syenogranite has geochemical characteristics of A-type granites that were mainly sourced from melting of juvenile crust. In comparison, the low-Mg-number diorite intrusion, with tholeiite and metaluminous features, was derived from young crust and mixed some mantle materials. The granodiorite and monzonite are both I-type granites, and are both sourced from the melting of juvenile crust. Based on a comprehensive analysis of previous geochronological, geochemical and isotopic data of magmatic and sedimentary rocks in the Bogda–Harlik belt, we consider that late Carboniferous intrusive rocks of the Bogda Mountains formed in an intra-arc extension related to a continent-based arc setting.

Keywords

U–Pb zircon agegeochemistryHf isotopeBogda Mountainstectonic setting
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 2 , February 2020 , pp. 289 - 306
Copyright
© Cambridge University Press 2019 

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References

Allen, MB, Sengor, AMC and Natal’in, BA (1995) Junggar, Turfan and Alakol basins as Late Permian to Early Triassic extensional structures in a sinistral shear zone in the Altaid orogenic collage, Central Asia. Journal of the Geological Society of London 152, 327–38.CrossRefGoogle Scholar
Allen, MB, Windley, BF and Zhang, C (1993) Paleozoic collisional tectonics and magmatism of the Chinese Tien Shan, central Asia. Tectonophysics 220, 89–115.CrossRefGoogle Scholar
BGMRXUAR (Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region) (1993) Regional Geology of Xinjiang Autonomous Region, Geological Memoirs, no. 32, Map Scale 1:500000. Beijing: Geological Publishing House (in Chinese).Google Scholar
Boynton, WV (1984) Geochemistry of the Rare Earth Elements: Meteorite Studies. In: Rare Earth Element Geochemistry (ed. Henderson, P), pp. 63–114. Elsevier.CrossRefGoogle Scholar
Carroll, AR, Graham, SA, Hendrix, MS, Ying, D and Zhou, D (1995) Late Paleozoic tectonic amalgamation of northwestern China: sedimentary record of the northern Tarim, northwestern Turpan, and southern Junggar basins. Geological Society of America Bulletin 107, 571–94.2.3.CO;2>CrossRefGoogle Scholar
Carroll, AR, Liang, Y, Graham, SA, Xiao, X, Hendrix, MS, Chu, J and Mcknight, CL (1990) Junggar basin, northwest China: trapped Late Paleozoic ocean. Tectonophysics 181, 1–14.CrossRefGoogle 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, DC, Zhao, XM and Deng, J (2010) U-Pb dating of Carboniferous sandstone detrital zircon from the north of the Bogda Mountains, eastern Xinjiang, and its geological significances. Acta Geologica Sinica 84, 1770–80.Google Scholar
Chen, JF, Guo, XS, Tang, JF and Zhou, TX (1999) Nd isotopic model ages: implications of the growth of the continental crust of southeastern China. Journal of Nanjing University (Nature Science) 35, 649–58 (in Chinese with English abstract).Google Scholar
Chen, X, Shu, L, Santosh, M and Zhao, X (2013) Island arc-type bimodal magmatism in the eastern Tianshan Belt, Northwest China: Geochemistry, zircon U–Pb geochronology and implications for the Paleozoic crustal evolution in Central Asia. Lithos 168–169, 48–66.CrossRefGoogle Scholar
Eby, GN (1990) The A-type granitoids: a review of their occurrence and chemical characteristics and speculations on their petrogenesis. Lithos 26, 115–34.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
Gu, LX, Hu, SX, Yu, CS, Li, HY, Xiao, XJ and Yan, ZF (2000) Carboniferous volcanites in the Bogda Mountains of eastern Tianshan: their tectonic implications. Acta Petrologica Sinica 16, 305–16 (in Chinese with English abstract).Google Scholar
Gu, LX, Hu, SX, Yu, CS, Zhao, M, Wu, CZ and Li, HY (2001) Intrusive activities during compression–extension tectonic conversion in the Bogda intracontinental orogen. Acta Petrologica Sinica 17, 187–98 (in Chinese with English abstract).Google Scholar
Han, BF, Guo, ZJ, Zhang, ZC, Zhang, L, Chen, JF and Song, B (2010) Age, geochemistry, and tectonic implications of a Late Paleozoic stitching pluton in the North Tian Shan suture zone, Western China. Geological Society of America Bulletin 122, 627–40.CrossRefGoogle Scholar
Hoskin, PWO and Black, LP (2000) Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. Journal of Metamorphic Geology 18, 423–39.CrossRefGoogle Scholar
Jahn, BM, Wu, FY and Chen, B (2000) 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
Jung, S, Hoernes, S and Mezger, K (2002) Synorogenic melting of mafic lower crust: constraints from geochronology, petrology and Sr, Nd, Pb and O isotope geochemistry of quartz diorites (Damara orogen, Namibia). Contributions to Mineralogy and Petrology 143, 551–66.CrossRefGoogle Scholar
Kröner, A, Kovach, V, Belousova, E, Hegner, E, Armstrong, R, Dolgopolova, A, Seltmann, R, Alexeiev, DV, Hoffmann, JE, Wong, J, Sun, M, Cai, K, Wang, T, Tong, Y, Wilde, SA, Degtyarev, KE and Rytsk, E (2014) Reassessment of continental growth during the accretionary history of the Central Asian Orogenic Belt. Gondwana Research 25, 103–25.CrossRefGoogle Scholar
Lei, W, Guo, JF, Ma, J, Xiao, L, Li, XC, Liu, J and Li, Y (2016a) Lithogeochemistry and LA-ICP-MS zircon U-Pb age and its tectonic significance of Sujishan A-type granite pluton, eastern Bogda Mountains. Geological Journal of China Universities 22, 231–41 (in Chinese with English abstract).Google Scholar
Li, P, Liu, W, Zhu, ZX, Chen, C, Jin, L, Xu, S and Chen, B (2013) Geochemical characteristics, geochronology and its geological significance of quartz diorite in Sangeshan area, west of Bogda, Xinjiang. Xinjiang Geology 31, 162–66 (in Chinese with English abstract).Google Scholar
Liang, T, Guo, XC, Gao, JG, Fan, TB, Qin, H, Zhou, RH and Huan, H (2011) Geochemistry and structure characteristic of carboniferous volcanic rocks in the eastern of Bogeda mountain. Xinjiang Geology 29, 289–95 (in Chinese with English abstract).Google Scholar
Liu, YS, Hu, ZC, Gao, S, Günther, D, Xu, J, Gao, CG and Chen, H (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, YS, Hu, ZC, Zong, KQ, Gao, CG and Shan, G (2010) Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Science Bulletin 55, 1535–46.CrossRefGoogle Scholar
Ludwig, KR (2003) ISOPLOT 3.0: A Geochronological Toolkit for Microsoft Excel. Berkeley, California: Berkeley Geochronology Center, Special Publication, 1–70 pp.Google Scholar
Ma, YF, Liu, YJ, Wang, Y, Tan, Z, Qian, C, Qin, T, Feng, ZQ, Sun, W and Zang, YQ (2019) Geochronology and geochemistry of the Carboniferous felsic rocks in the central Great Xing’an Range, NE China: Implications for the amalgamation history of Xing’an and Songliao-Xilinhot blocks. Geological Journal 54, 482–513.CrossRefGoogle Scholar
Maniar, PD and Piccoli, PM (1989) Tectonic discrimination of granitoids. Geological Society of American Bulletin 101, 635–43.2.3.CO;2>CrossRefGoogle Scholar
Middlemost, EAK (1994) Naming materials in the magma/igneous rock system. Earth Science Reviews 37, 215–24.CrossRefGoogle Scholar
Patiño, Douce AE and Johnston, AD (1991) Phase equilibria and melt productivity in the pelitic system: implications for the origin of peraluminous granitoids and aluminous granulites. Contributions to Mineralogy and Petrology 107, 202–18.CrossRefGoogle Scholar
Peccerillo, A and Taylor, AR (1976) Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey. Contributions to Mineralogy and Petrology 58, 63–81.CrossRefGoogle Scholar
Pirajno, F, Mao, JW, Zhang, ZC, Zhang, ZH and Chai, FM (2008) The association of mafic–ultramafic intrusions and A-type magmatism in the Tianshan and Altay orogens, NW China: implications for geodynamic evolution and potential for the discovery of new ore deposits. Journal of Asian Earth Sciences 32, 165–83.CrossRefGoogle Scholar
Qin, KZ, Su, BX, Sakyi, PA, Tang, DM, Li, XH, Sun, H, Xiao, QH and Liu, PP (2011) SIMS zircon U–Pb geochronology and Sr–Nd isotopes of Ni–Cu-bearing mafic–ultramafic intrusions in Eastern Tianshan and Beishan in correlation with flood basalts in Tarim Basin (NW China): constraints on a ca. 280 Ma mantle plume. American Journal of Science 311, 237–60.CrossRefGoogle Scholar
Rapp, RP 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
Searle, MP, Parrish, RR, Hodges, KV, Hurford, A, Ayres, MW and Whitehouse, MJ (1997) Shisha Pangma Leucogranite, South Tibetan Himalaya: field relations, geochemistry, age, origin, and emplacement. Journal of Geology 105, 295–318.CrossRefGoogle Scholar
Shu, L, Wang, B, Zhu, W, Guo, Z, Charvet, J and Zhang, Y (2011) Timing of initiation of extension in the Tianshan, based on structural, geochemical and geochronological analyses of bimodal volcanism and olistostrome in the Bogda Shan (NW China). International Journal of Earth Sciences 100, 1647–63.CrossRefGoogle Scholar
Shu, LS, Zhu, WB, Wang, B, Faure, M, Charvet, J and Cluzel, D (2005) The post-collision intracontinental rifting and olistostrome on the southern slope of Bogda Mountains, Xinjiang. Acta Petrologica Sinica 21, 25–36 (in Chinese with English abstract).Google Scholar
Si, G, Su, H, Yang, G, Zhang, C and Yang, G (2014) Geological significance and geochemical characteristics of the Sikeshu pluton in north Tianshan, Xinjiang. Xinjiang Geology 32, 19–24 (in Chinese with English abstract).Google Scholar
Su, BX, Qin, KZ, Sun, H, Tang, DM, Sakyi, PA, Chu, ZY and Xiao, QH (2012) Subduction-induced mantle heterogeneity beneath Eastern Tianshan and Beishan: Insights from Nd–Sr–Hf–O isotopic mapping of Late Paleozoic mafic–ultramafic complexes. Lithos 134–135, 41–51.Google Scholar
Sun, G, Li, J, Gao, L and Yang, T (2005) Zircon SHRIMP U–Pb age of a dioritic pluton in the Harlik Mountain, Eastern Xinjiang, and its tectonic implication. Geological Review 51, 463–69 (in Chinese with English abstract).Google Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Magmatism In Ocean Basins (eds Saunders, AD and Norry, MJ), pp. 313–45. Geological Society of London, Special Publication no. 42.Google Scholar
Wali, G, Wang, B, Cluzel, D and Zhong, L (2018) Carboniferous-Early Permian magmatic evolution of the Bogda Range (Xinjiang, NW China): Implications for the Late Paleozoic accretionary tectonics of the SW Central Asian Orogenic Belt. Journal of Asian Earth Sciences 153, 238–51.CrossRefGoogle Scholar
Wang, B, Shu, L, Faure, M, Jahn, BM, Cluzel, D, Charvet, J, Chung, Sl and Meffre, S (2011) Paleozoic tectonics of the southern Chinese Tianshan: insights from structural, chronological and geochemical studies of the Heiyingshan ophiolitic mélange (NW China). Tectonophysics 497, 85–104.CrossRefGoogle Scholar
Wang, C, Chen, B, Ma, XH and Yan, XL (2015) Petrogenesis of early and late Paleozoic plutons in Sanchakou area of east Tianshan and their implications for evolution of Kangur Suture Zone. Journal of Earth Sciences Environment 37, 52–70 (in Chinese with English abstract).Google Scholar
Wang, C, Ma, XH, Chen, B and Yan, XL (2017) Late Carboniferous volcanism of the Harlik orogenic belt, Xinjiang: Zircon U-Pb geochronological, geochemical and Sr-Nd isotopic evidence. Acta Petrologica Sinica 33, 440–54 (in Chinese with English abstract).Google 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
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
Winchester, JA and Floyd, PA (1976) Geochemical magma type discrimination: application to altered and metamorphosed basic igneous rocks. Earth and Planetary Science Letters 28, 459–69.CrossRefGoogle Scholar
Wood, DA (1980) The application of a Th–Hf–Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British tertiary volcanic province. Earth & Planetary Science Letters 50, 11–30.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, Zhao, GC, Sun, DY, Wilde, SA and Yang, JH (2007) The Hulan Group: Its role in the evolution of the Central Asian Orogenic Belt of NE China. Journal of Asian Earth Sciences 30, 542–56.CrossRefGoogle Scholar
Wu, YS, Chen, YJ and Zhou, KF (2016) Mo deposits in Northwest China: Geology, geochemistry, geochronology and tectonic setting. Ore Geology Reviews 81, 641–71.CrossRefGoogle Scholar
XBGMR (Xinjiang Bureau of Geology and Mineral Resources) (1988) Geological Map 1:200000, Dabancheng-Tuokexun Sheet (L-45-5 and L-45-11).Google Scholar
Xia, LQ, Xia, ZC, Xu, XY, Li, XM, Ma, ZP and Wang, LS (2004) Carboniferous Tianshan igneous megaprovince and mantle plume. Geological Bulletin of China 23, 903–10 (in Chinese with English abstract).Google Scholar
Xiao, B, Chen, H, Hollings, P, Han, JS, Wang, YF, Yang, JT and Cai, KD (2017) Magmatic evolution of the Tuwu-Yandong porphyry Cu belt, NW China: constraints from geochronology, geochemistry and Sr-Nd-Hf isotopes. Gondwana Research 43, 74–91.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Allen, MB and Han, C (2013) Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage. Gondwana Research 23, 1316–41.CrossRefGoogle Scholar
Xiao, WJ, Zhang, LC, Qin, KZ, Sun, S and Li, JL (2004) Paleozoic accretionary and collisional tectonics of the eastern Tianshan (China): implications for the continental growth of Central Asia. American Journal of Science 304, 370–95.CrossRefGoogle Scholar
Xie, W, Luo, ZY, Xu, YG, Chen, YB, Hong, LB, Ma, L and Ma, Q (2016a). Petrogenesis and geochemistry of the Late Carboniferous rear-arc (or back-arc) pillow basaltic lava in the Bogda Mountains, Chinese North Tianshan. Lithos 244, 30–42.CrossRefGoogle Scholar
Xie, W, Xu, YG, Chen, YB, Luo, ZY, Hong, LB, Ma, L and Liu, HQ (2016b) High-alumina basalts from the Bogda Mountains suggest an arc setting for Chinese Northern Tianshan during the Late Carboniferous. Lithos 256–257, 165–81.CrossRefGoogle Scholar
Xie, W, Xu, YG, Luo, ZY, Liu, HQ, Hong, LB and Ma, L (2016c) Petrogenesis and geodynamic implications of the Late Carboniferous felsic volcanics in the Bogda belt, Chinese Northern Tianshan. Gondwana Research 39, 165–79.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
Yakubchuk, A (2017) Evolution of the Central Asian Orogenic Supercollage since Late Neoproterozoic revised again. Gondwana Research 2017, 47.Google Scholar
Yuan, C, Sun, M, Wilde, S, Xiao, W, Xu, Y, Long, X and Zhao, G (2010) Post-collisional plutons in the Balikun area, East Chinese Tianshan: Evolving magmatism in response to extension and slab break-off. Lithos 119, 269–88.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, HX, Niu, HC, Terada, K, Yu, XY, Sato, H and Ito, J (2003) Zircon SHRIMP U-Pb dating on plagiogranite from Kuerti ophiolite in Altay, North Xinjiang. Chinese Science Bulletin 48, 2231–2235 (in Chinese with English abstract).CrossRefGoogle Scholar
Zhao, TY, Xu, SQ, Zhu, ZX, Liu, X and Chen, C (2014) Geological and geochemical features of carboniferous volcanic rocks in Bogda-Harlik Mountains, Xinjiang and their tectonic significance. Geological Review 60, 115–24 (in Chinese with English abstract).Google Scholar