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Petrogenesis and tectonic implications of the Early Carboniferous shoshonitic to calc-alkaline magmatic rocks of the southern Yili terrane, western Tianshan

Published online by Cambridge University Press:  04 April 2023

Hao Xing Open the ORCID record for Hao Xing [Opens in a new window] ,
Chunji Xue ,
Xiaobo Zhao ,
DTA Symons  and
Pengqiao Niu
Hao Xing
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, School of Earth Sciences, East China University of Technology, Nanchang, Jiangxi 330013, China
Chunji Xue*
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resource, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China The National 305 Project Office of Xinjiang, Urumqi 830000, China
Xiaobo Zhao
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resource, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
DTA Symons
Affiliation:
School of the Environment, University of Windsor, Windsor, N9B 3P4, Canada
Pengqiao Niu
Affiliation:
State Key Laboratory of Nuclear Resources and Environment, School of Earth Sciences, East China University of Technology, Nanchang, Jiangxi 330013, China
*
Author for correspondence: Chunji Xue, Email: chunji.xue@cugb.edu.cn
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Abstract

In the Yili terrane at Awulale mountain, most shoshonitic lavas are related to post-collision extension and were extruded during the Late Carboniferous to Early Permian (310–280 Ma). Herein, we evaluate a small-volume occurrence of shoshonitic magmas in the southern Yili terrane formed c. 346 Ma ago. The high MgO (Mg#) and positive Hf isotope values of the shoshonitic magmas indicate the input of juvenile mantle-derived material. Still, their high Ba–Sr signatures were likely inherited from the partial melting of previously metasomatized lithospheric mantle. We argue the shoshonitic magmatic activity recorded a syn-subduction extensional history in the Yili terrane. This interpretation is consistent with the magmatic records from Early Carboniferous A-type granite and magnesian andesite found in the Zhaosu–Adentao–Dahalajunshan area of the southern Yili terrane. Combined with the geological development in this area, we propose that the emergence of the shoshonitic rocks records either the retreat of the trench or the rollback of the Junggar oceanic slab that occurred at or before the 346.1 ± 3.1 Ma age of the rocks.

Keywords

shoshonitic volcanic rocksslab rollbacktectonic settingXinyuanYili terrane
Type
Original Article
Information
Geological Magazine , Volume 160 , Issue 5 , May 2023 , pp. 855 - 873
Copyright
© The Author(s), 2023. Published by Cambridge University Press

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References

Altherr, R, Holl, A, Hegner, E, Langer, C and Kreuzer, H (2000) High-potassium, calc-alkaline I-type plutonism in the European variscides: northern Vosges (France) and northern Schwarald (Germany). Lithos 50, 51–73.CrossRefGoogle Scholar
An, F, Zhu, YF, Wei, SN and Lai, SC (2013) An Early Devonian to Early Carboniferous volcanic arc in North Tianshan, NW China: geochronological and geochemical evidence from volcanic rocks. Journal of Asian Earth Sciences 78, 100–13.CrossRefGoogle Scholar
Andersen, T (2002) Correction of common Pb in U-Pb analyses that do not report 204Pb. Chemical Geology 192, 59–79.CrossRefGoogle Scholar
Avanzinelli, R, Lustrino, M, Mattei, M, Melluso, L and Conticelli, S (2009) Potassic and ultrapotassic magmatism in the circum-Tyrrhenian region: significance of carbonated pelitic vs. pelitic sediment recycling at destructive plate margins. Lithos 113, 213–27.CrossRefGoogle Scholar
Beccaluva, L, Bianchini, G, Mameli, P and Natali, C (2013) Miocene shoshonite volcanism in Sardinia: implications for magma sources and geodynamic evolution of the central-western Mediterranean. Lithos 180–181, 128–37.CrossRefGoogle Scholar
Blichert-Toft, J and Albarède, F (1997) The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth and Planetary Science Letters 148, 243–58.CrossRefGoogle 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.CrossRefGoogle Scholar
Campbell, IH, Stepanov, AS, Liang, HY, Allen, CM, Norman, MC, Zhang, YQ and Xie, YW (2014) The origin of shoshonites: new insights from the Tertiary high-potassic intrusions of eastern Tibet. Lithos 167, 1–22.Google Scholar
Cao, YC, Wang, B, Jahn, BM, Cluzel, D, Shu, LS and Zhong, LL (2017) Late Paleozoic arc magmatism in the southern Yili Block (NW China): insights to the geodynamic evolution of the Balkhash-Yili continental margin, Central Asian Orogenic Belt. Lithos 278–281, 111–25.CrossRefGoogle Scholar
Carr, MJ, Feigenson, MD and Bennett, EA (1990) Incompatible element and isotopic evidence for tectonic control of source mixing and melt extraction along the Central American arc. Contributions to Mineralogy and Petrology 105, 369–80.CrossRefGoogle Scholar
Castillo, PR, Janney, PE and Solidum, RU (1999) Petrology and geochemistry of Camiguin Island, southern Philippines: insights to the source of adakites and other lavas in a complex arc setting. Contributions to Mineralogy and Petrology 134, 33–51.CrossRefGoogle Scholar
Castro, A, Aghazadeh, M, Badrzadeh, Z and Chichorro, M (2013) Late Eocene-Oligocene post-collisional monzonitic intrusions from the Alborz magmatic belt, NW Iran: an example of monzonite magma generation from a metasomatized mantle source. Lithos 180–181, 109–27.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
Collins, W, Beams, S, White, A and Chappell, B (1982) Nature and origin of A-type granites with particular reference to southeastern Australia. Contributions to Mineralogy and Petrology 80, 189–200.CrossRefGoogle Scholar
Cullen, JT, Field, MPM and Sherrell, RM (2001) Determination of trace elements in filtered suspended marine particulate material by sector field HR-ICP-MS. Journal of Analytical Atomic Spectrometry 16, 1307–12.CrossRefGoogle Scholar
Defant, MJ and Kepezhinskas, P (2001) Evidence suggests slab melting in arc magmas. Eos, Transactions of the American Geophysical Union 82, 65–9.CrossRefGoogle Scholar
Dufek, J and Bergantz, GW (2005) Lower crustal magma genesis and preservation: a stochastic framework for the evaluation of basalt-crust interaction. Journal of Petrology 46, 2167–95.CrossRefGoogle Scholar
Feng, WY and Zhu, YF (2019) Petrogenesis and tectonic implications of the Late Carboniferous calc-alkaline and shoshonitic magmatic rocks in the Awulale mountain, western Tianshan. Gondwana Research 76, 44–61.CrossRefGoogle Scholar
Feng, WY and Zhu, YF (2020) Petrology and geochemistry of Early Carboniferous volcanic rocks in the Xinyuan region of western Tianshan: implications for magma sources. Lithos 364–365, 105505 CrossRefGoogle Scholar
Foley, S (1992) Vein-plus-wall-rock melting mechanisms in the lithosphere and the origin of potassic alkaline magmas. Lithos 28, 435–53.CrossRefGoogle Scholar
Gao, J, Long, LL, Qian, Q, Huang, DZ, Su, W and Klemd, R (2006) South Tianshan: a Late Paleozoic or Triassic orogen? Acta Petrologica Sinica 22, 1049–61.Google Scholar
Gill, RCO, Aparicio, A, El Azzouzi, M, Hernandez, J, Thirlwall, MF, Bourgois, J and Marriner, GF (2004) Depleted arc volcanism in the Alboran Sea and shoshonitic volcanism in Morocco: geochemical and isotopic constraints on Neogene tectonic processes. Lithos 78, 363–88.CrossRefGoogle Scholar
Han, YG and Zhao, GC (2018) Final amalgamation of the Tianshan and Junggar orogenic collage in the southwestern Central Asian Orogenic Belt: constraints on the closure of the Paleo-Asian Ocean. Earth-Science Reviews 186, 129–52.CrossRefGoogle Scholar
Hermann, J and Rubatto, D (2009) Accessory phase control on the trace element signature of sediment melts in subduction zones. Chemical Geology 265, 512–26.CrossRefGoogle Scholar
Hoskin, PWO and Schaltegger, U (2003) The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry 53, 27–62.CrossRefGoogle Scholar
Hou, KJ, Li, YH, Zou, TR, Qu, XM, Shi, YR and Xie, GQ (2007) Laser ablation-MCICP-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
Huang, H, Wang, T, Tong, Y, Qin, Q, Ma, XX and Yin, JY (2020) Rejuvenation of ancient micro-continents during accretionary orogenesis: insights from the Yili Block and adjacent regions of the SW Central Asian Orogenic Belt. Earth-Science Reviews 208, 103–255.CrossRefGoogle Scholar
Jackson, SE, Pearson, NJ, Griffin, WL and Belousova, EA (2004) The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology 211, 47–69.CrossRefGoogle Scholar
Kay, RW and Kay, SM (1993) Delamination and delamination magmatism. Tectonophysics 219, 177–89.CrossRefGoogle Scholar
Kelemen, PB, Hanghj, K and Greene, AR (2003) One view of the geochemistry of subduction-related magmatic arcs, with an emphasis on primitive andesite and lower crust. Treatise on Geochemistry 3, 593–659.Google Scholar
Keskin, M, Genç, ŞC and Tüysüz, O (2008) Petrology and geochemistry of post-collisional Middle Eocene volcanic units in North-Central Turkey: evidence for magma generation by slab breakoff following the closure of the Northern Neotethys Ocean. Lithos 104, 267–305.CrossRefGoogle Scholar
Lee, CTA and Bachmann, O (2014) How important is the role of crystal fractionation in making intermediate magmas? Insights from Zr and P systematics. Earth and Planetary Science Letters 393, 266–74.CrossRefGoogle Scholar
Li, HK, Geng, JZ, Hao, S, Zhang, YQ and Li, HM (2009) Determination of U-Pb isotopic age of zircon by Laser ablation multi receiver plasma mass spectrometer (LA-MC-ICPMS). Acta Mineralogica Sinica 29, 600–1 (in Chinese).Google Scholar
Li, JL, Qian, Q, Gao, J, Su, W, Zhang, X, Liu, X and Jiang, T (2010) Geochemistry zircon U-Pb ages and tectonic settings of the Dahalajunshan volcanics and granitic intrusions from the Adengtao area in the southeast Zhaosu, western Tianshan Mountains. Acta Petrologica Sinica 26, 2913–24 (in Chinese with English abstract).Google Scholar
Li, JL, Su, W, Zhang, X and Liu, X (2009) Zircon Cameca U-Pb dating and its significance for granulite-facies gneisses from the western Awulale Mountains, Western Tianshan, China. Geological Bulletin of China 28, 1852–62 (in Chinese with English abstract).Google Scholar
Li, WX, Li, XH, Wang, XC and Yang, DS (2017) Petrogenesis of Cretaceous shoshonitic rocks in the northern Wuyi Mountains, South China: a result of the roll-back of a flat-slab? Lithos 288–289, 125–42.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 orogeny: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths. Journal of Petrology 51, 537–71.CrossRefGoogle Scholar
Long, LL, Gao, J, Klemd, R, Beier, C, Qian, Q, Zhang, X, Wang, JB and Jiang, T (2011) Geochemical and geochronological studies of granitoid rocks from the Western Tianshan Orogen: implications for continental growth in the southwestern Central Asian Orogenic Belt. Lithos 126, 321–40.CrossRefGoogle Scholar
Long, LL, Gao, J, Xiong, XM and Qian, Q (2006) The geochemical characteristics and the age of the Kule Lake ophiolite in the southern Tianshan. Acta Petrologica Sinica 22, 65–73 (in Chinese with English abstract).Google Scholar
Ludwig, KR (2003) ISOPLOT 3.00: A Geochronology Toolkit for Microsoft Excel. Berkeley, California: Berkeley Geochronological Center Special Publication, 53 pp.Google Scholar
Manley, CR, Glazner, AF and Farmer, GL (2000) Timing of volcanism in the Sierra Nevada of California: evidence for Pliocene delamination of the batholithic root? Geology 28, 811–14.2.0.CO;2>CrossRefGoogle Scholar
Morrison, GW (1980) Characteristics and tectonic setting of the shoshonite rock association. Lithos 13, 97–108.CrossRefGoogle Scholar
Omrani, J, Agard, P, Whitechurch, H, Benoit, M, Prouteau, G and Jolivet, L (2008) Arc-magmatism and subduction history beneath the Zagros Mountains, Iran: a new report of adakites and geodynamic consequences. Lithos 106, 380–98.CrossRefGoogle Scholar
Pe-Piper, G, Piper, DJW, Koukouvelas, I, Dolansky, LM and Kokkalas, S (2009) Post-orogenic shoshonitic rocks and their origin by melting underplated basalts: the Miocene of Limnos, Greece. Geological Society of America Bulletin 121, 39–54.Google Scholar
Petford, N and Atherton, M (1996) Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith, Peru. Journal of Petrology 37, 1491–521.CrossRefGoogle Scholar
Portnyagin, M, Hoernle, K, Plechov, P, Mironov, N and Khubunaya, S (2007) Constraints on mantle melting and composition and nature of slab components in volcanic arcs from volatiles and trace elements in melt inclusions from the Kamchatka Arc. Earth and Planetary Science Letters 255, 63–9.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
Richards, JP and Kerrich, R (2007) Special paper. Adakite-like rocks: their diverse origins and questionable role in metallogenesis. Economic Geology 102, 537–76.CrossRefGoogle Scholar
Ru, YJ (2012) The stratigraphic sequanence, petrogenesis and tectonic setting of the volcanic rocks of the Dahalajunshan Formation, western Tianshan Mountani, China. Master degree of Chang’an University, pp. 1–113 (in Chinese with English abstract).Google Scholar
Saunders, AD, Rogers, G, Marriner, GF, Terrell, DJ and Verma, SP (1987) Geochemistry of Cenozoic volcanic rocks, Baja California, Mexico: implications for the petrogenesis of post-subduction magmas. Journal of Volcanology and Geothermal Research 32, 223–45.CrossRefGoogle Scholar
Sisson, TW, Ratajeski, K, Hankins, WB and Glazner, AF (2005) Voluminous granitic magmas from common basaltic sources. Contributions to Mineralogy and Petrology 148, 635–61.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
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
Tan, Z, Agard, P, Patrick, M, Gao, J, John, T, Léa, B, Jiang, T, Wang, XS, Hong, T, Wan, B and Caron, B (2019) Architecture and P-T-deformation-time evolution of the Chinese SW-Tianshan HP/UHP complex: implications for subduction dynamics. Earth-Science Reviews 197, 102894.CrossRefGoogle Scholar
Tarney, J and Jones, CE (1994) Trace element geochemistry of orogenic igneous rocks and crustal growth models. Journal of the Geological Society 151, 855–68.CrossRefGoogle Scholar
Taylor, SR and McLennan, SM (1985) The Continental Crust: Its Composition and Evolution. Oxford: Blackwell.Google 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, S, Hawkesworth, C, Liu, JQ, Rogers, N, Kelley, S and van Calsteren, P (1993) Timing of Tibetan uplift constrained by analysis of volcanic rocks. Nature 364, 50–4.CrossRefGoogle Scholar
Vigouroux, N, Wallace, PJ and Kent, AJR (2008) Volatiles in high-K magmas from the western Trans-Mexican Volcanic Belt: evidence for fluid fluxing and extreme enrichment of the mantle wedge by subduction processes. Journal of Petrology 49, 12–5.CrossRefGoogle Scholar
Wang, B, Chen, Y, Zhan, S, Shu, LS, Michel, F, Cluzel, D, Charvet, J and Laurent-Charvet, S (2007) Primary Carboniferous and Permian paleomagnetic results from the Yili Block (NW China) and their implications on the geodynamic evolution of Chinese Tianshan Belt. Earth and Planetary Science Letters 263, 288–308.CrossRefGoogle Scholar
Wang, B, Cluzel, D, Shu, LS, Faure, M, Charvet, J, Chen, Y, Meffre, S and de Jong, K (2009) Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transcurrent tectonics, western Chinese Tianshan. International Journal of Earth Science 98, 1275–98.Google Scholar
Wang, B, Liu, HS, Shu, LS, Jahn, BM, Chung, SL, Zhai, YZ and Liu, DY (2014) Early Neoproterozoic crustal evolution in northern Yili Block: insights from migmatite, orthogneiss and leucogranite of the Wenquan metamorphic complex in the NW Chinese Tianshan. Precambrian Research 242, 58–81.CrossRefGoogle Scholar
Wang, W, Zeng, LS, Gao, LE, Wang, Q, Guo, C, Hou, KJ and Zeng, JL (2018) Eocene-Oligocene potassic high Ba-Sr granitoids in the Southeastern Tibet: petrogenesis and tectonic implications. Lithos 322, 38–51.CrossRefGoogle Scholar
Wang, ZP, Li, YJ, Yang, GX, Tong, LL, Li, H, Luo, YQ and Liu, Y (2020) Petrogenesis and geochemical characteristics of Early Carboniferous sanukitic high-Mg andesite from Atengtao Mountain, Yili Block: implications for the tectonic setting during Late Paleozoic in Chinese West Tianshan. Geological Journal 55, 517–32.CrossRefGoogle Scholar
Windley, BF, Alexeiev, D, Xiao, WJ, Kroner, A and Badarch, G (2007) Tectonic models for accretion of the Central Asian Orogenic Belt. Journal of the Geological Society 164, 31–47.CrossRefGoogle Scholar
XBGMR (Xinjiang Bureau of Geology and Mineral Resources) (1993) Regional Geology of Xinjiang Uygur Autonomy Region. Beijing: Geology Publishing House, 841 pp. (in Chinese with English abstract).Google Scholar
Xia, LQ and Li, XM (2020) Revisiting the tectonic setting of the Carboniferous volcanic rocks in the Chinese Tianshan and its neighboring areas. Gondwana Research 84, 1–19.CrossRefGoogle Scholar
Xia, LQ, Xu, XY, Li, XM, Ma, ZP and Xia, ZC (2012) Reassessment of petrogenesis of Carboniferous-Early Permian rift-related volcanic rocks in the Chinese Tianshan and its neighboring areas. Geoscience Frontiers 3, 445–71.CrossRefGoogle Scholar
Xing, H, Xue, CJ, Chi, GX, Zhao, XB, Liu, C, Man, RH and Symons, DTA (2021) Petrogenesis of volcanic rocks of the Devonian-Carboniferous Dahalajunshan Formation, Western Tianshan: implications for crustal growth in an accretionary orogen. Lithos 386–387, 106003.CrossRefGoogle Scholar
Xu, XY, Li, XM, Ma, ZP, Xia, LQ, Xia, ZC and Pen, GX (2006) LA-ICP-MS zircon U-Pb dating of gabbro from the Bayingou ophiolite in the northern Tianshan Mountains. Acta Geologica Sinica 80, 1168–76.Google Scholar
Xu, XY, Wang, HL, Li, P, Chen, JL, Ma, ZP, Zhu, T, Wang, N and Dong, YP (2013) Geochemistry and geochronology of Paleozoic intrusions in the Nalati (Narati) area in western Tianshan, Xinjiang, China: implications for Paleozoic tectonic evolution. Journal of Asian Earth Sciences 72, 33–62.CrossRefGoogle Scholar
Yang, WB, Niu, HC, Shan, Q, Luo, Y, Sun, WD, Li, CY, Li, NB and Yu, XY (2012) Late Paleozoic calc-alkaline to shoshonitic magmatism and its geodynamic implications, Yuximolegai area, western Tianshan, Xinjiang. Gondwana Research 22, 325–40.CrossRefGoogle Scholar
Yin, JY, Chen, W, Xiao, WJ, Yuan, C, Zhang, B, Cai, KD and Long, XP (2016) Geochronology, petrogenesis and tectonic significance of the Latest Devonian-Early Carboniferous I-type granites in the Central Tianshan, NW China. Gondwana Research 47, 188–99.CrossRefGoogle Scholar
Yu, XQ, Wang, ZX, Zhou, X, Xiao, WF and Yang, XP (2016) Zircon U–Pb geochronology and Sr–Nd isotopes of volcanic rocks from the Dahalajunshan Formation: implications for Late Devonian–Middle Carboniferous tectonic evolution of the Chinese Western Tianshan. International Journal of Earth Sciences 105, 1637–61.CrossRefGoogle Scholar
Zhao, XB, Xue, CJ, Chi, GX, Wang, HG and Qi, TJ (2014) Epithermal Au and polymetallic mineralization in the Tulasu Basin, western Tianshan, NW China: potential for the discovery of porphyry Cu-Au deposits. Ore Geology Reviews 60, 76–96.CrossRefGoogle Scholar
Zhao, ZH, Bai, ZH, Xiong, XL, Mei, HJ and Wang, YX (2003) 40Ar/39Ar chronological study of Late Paleozoic volcanic-hypabyssal igneous rocks in western Tianshan, Xinjiang. Geochemica 32, 317–27 (in Chinese with English abstract).Google Scholar
Zhu, YF, An, F, Xue, YX, Chen, B and Zhang, LF (2010) Zircon U-Pb age for Kesang Rondong volcanic rocks, Southwest Tianshan Mts, Tekes, Xinjiang. Acta Petrologica Sinica 26, 2255–63 (in Chinese with English abstract).Google Scholar
Zhu, YF, Guo, X, Song, B, Zhang, LF and Gu, LB (2009) Petrology, Sr-Nd-Hf isotopic geochemistry and zircon chronology of the Late Paleozoic volcanic rocks in the southwestern Tianshan Mountains, Xinjiang, NW China. Journal of the Geological Society 166, 1085–99.CrossRefGoogle Scholar
Zhu, YF, Zhang, LF, Gu, LB, Guo, X and Zhou, J (2005) Study on trace element geochemistry and SHRIMP chronology of Carboniferous volcanic rocks in Western Tianshan. Chinese Science Bulletin 50, 2004–14 (in Chinese).CrossRefGoogle Scholar
Zu, B, Seltmann, R, Xue, CJ, Wang, T, Dolgopolova, A, Li, C, Zhou, LM, Pak, N, Ivleva, E, Chai, MC and Zhao, XB (2019) Multiple episodes of Late Paleozoic Cu-Au mineralization in the Chatkal-Kurama terrane: new constraints from the Kuru-Tegerek and Bozymchak skarn deposits, Kyrgyzstan. Ore Geology Reviews 113, 103077.CrossRefGoogle Scholar
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