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A mid-Palaeozoic ocean–continent transition in the Mazongshan subduction–accretion complex, Beishan, NW China: new structural, chemical and age data constrain the petrogenesis and tectonic evolution

Published online by Cambridge University Press:  21 April 2020

J.-X. Wang ,
K.-X. Zhang Open the ORCID record for K.-X. Zhang [Opens in a new window] ,
Brian F. Windley ,
B.-W. Song ,
X.-H. Kou ,
S.-D. Wang  and
L.-J. Wang
J.-X. Wang
Affiliation:
School of Earth Sciences, China University of Geosciences, Wuhan430074, China State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan430074, China
K.-X. Zhang*
Affiliation:
School of Earth Sciences, China University of Geosciences, Wuhan430074, China State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan430074, China Institute of Geological Survey, China University of Geosciences, Wuhan430074, China
Brian F. Windley
Affiliation:
Department of Geology, University of Leicester, LeicesterLE1 7RH, UK
B.-W. Song
Affiliation:
Institute of Geological Survey, China University of Geosciences, Wuhan430074, China
X.-H. Kou
Affiliation:
Institute of Geological Survey, China University of Geosciences, Wuhan430074, China
S.-D. Wang
Affiliation:
Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang065000, China
L.-J. Wang
Affiliation:
School of Earth Sciences, China University of Geosciences, Wuhan430074, China State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan430074, China
*
Author for correspondence: K.-X. Zhang, Email: [email protected]
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Abstract

Accretionary orogens contain key evidence for the conversion of oceanic to continental crust. The late tectonic history and closure time of the Palaeo-Asian Ocean are recorded in the Mazongshan subduction–accretion complex in the southern Beishan margin of the Central Asian Orogenic Belt. We present new data on the structure, petrology, geochemistry and zircon U–Pb isotope ages of the Mazongshan subduction–accretion complex, which is a tectonic mélange with a block-in-matrix structure. The blocks are of serpentinized peridotite, basalt, gabbro, basaltic andesite, chert and seamount sediments within a matrix that is mainly composed of fore-arc-trench turbidites. U–Pb zircon ages of two gabbros are 454.6 ± 2.5 Ma and 434.1 ± 3.6 Ma, an andesite has a U–Pb zircon age of 451.3 ± 3.5 Ma and a tuffaceous slate has the youngest U–Pb zircon age of 353.6 ± 5.1 Ma. These new isotopic ages, combined with published data on ophiolitic mélanges from central Beishan, indicate that the subduction–accretion of Beishan in the southernmost Central Asian Orogenic Belt lasted until Late Ordovician – Early Carboniferous time. Structure and age data demonstrate that the younging direction of accretion was southwards and that the subduction zone dipped continuously to the north. Accordingly, these results record the conversion of oceanic to continental crust in the southern Beishan accretionary collage.

Keywords

subduction–accretion mélangemagmatic arcsBeishan accretionary collageCentral Asian Orogenic Belt
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 11 , November 2020 , pp. 1877 - 1897
Copyright
© Cambridge University Press 2020

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References

Anonymous (1972) Ophiolites. Geotimes 17, 24–5.Google Scholar
Ao, SJ, Xiao, WJ, Han, CM, Li, XH, Qu, JF, Zhang, JE, Guo, QQ and Tian, ZH (2012) Cambrian to early Silurian ophiolite and accretionary processes in the Beishan collage, NW China: implications for the architecture of the Southern Altaids. Geological Magazine 149, 606–25.CrossRefGoogle Scholar
Ao, SJ, Xiao, WJ, Windley, BF, Mao, QG, Han, CM, Zhang, JE, Yang, LK and Geng, JZ (2016) Paleozoic accretionary orogenesis in the eastern Beishan orogen: constraints from zircon U–Pb and 40Ar/39Ar geochronology. Gondwana Research 30, 224–35.CrossRefGoogle Scholar
Brenan, JM, Shaw, HF and Ryerson, FJ (1995) Experimental evidence for the origin of lead enrichment in convergent-margin magmas. Nature 378, 54–6.CrossRefGoogle Scholar
Brown, EH and Gehrels, GE (2007) Detrital zircon constraints on terrane ages and affinities and timing of orogenic events in the San Juan Islands and North Cascades, Washington. Canadian Journal of Earth Sciences 44, 1375–96.CrossRefGoogle Scholar
Castillo, P, Solidum, R and Punongbayan, R (2002) Origin of high field strength element enrichment in the Sulu Arc, southern Philippines, revisited. Geology 30, 707–10.2.0.CO;2>CrossRefGoogle Scholar
Cawood, PA, Kröner, A, Collins, WJ, Kusky, TM, Mooney, WD and Windley, BF (2009) Accretionary orogens through Earth history. In Earth Accretionary Systems in Space and Time (eds Cawood, PA and Kröner, A), pp. 1–36. Geological Society of London, Special Publication no. 318.Google Scholar
Chen, C, Xiu, D, Pan, ZL, Zhang, H, Zhang, JL, Li, QZ and Zhuan, SP (2017) Early Paleozoic crustal extensional tectonic regime in the central part of Beishan Orogenic Belt: new evidence from geochronology and geochemistry of gabbro in Shibanjing. Acta Geologica Sinica 91, 1661–73 (in Chinese with English abstract).Google Scholar
Condie, K (2007) Accretionary orogens in space and time. In 4-D Framework of Continental Crust (eds Hatcher, RD , Jr, Carlson, MP, McBride, JH and Martínez Catalán, JR), pp. 145–58. Geological Society of America, Boulder, Memoir no. 200.CrossRefGoogle Scholar
Davidson, JP and Arculus, RJ (2006) The significance of Phanerozoic arc magmatism in generating continental crust. In Evolution and Differentiation of the Continental Crust (eds Brown, M and Rushmer, T), pp. 135–72. Cambridge: Cambridge University Press.Google Scholar
Davies, JH and Stevenson, DJ (1992) Physical model of source region of subduction zone volcanics. Journal of Geophysical Research: Solid Earth 97, 2037–70.CrossRefGoogle Scholar
Degtyarev, KE (2011) Tectonic evolution of Early Paleozoic island-arc systems and continental crust formation in the Caledonides of Kazakhstan and the North Tien Shan. Geotectonics 45, 23–50.CrossRefGoogle Scholar
Dickinson, WR and Gehrels, GE (2009) Use of U–Pb ages of detrital zircons to infer maximum depositional ages of strata: A test against a Colorado Plateau Mesozoic database. Earth and Planetary Science Letters 288, 115–25.CrossRefGoogle Scholar
Dilek, Y and Furnes, H (2011) Ophiolite genesis and global tectonics: geochemical and tectonic fingerprinting of ancient oceanic lithosphere. Geological Society of America Bulletin 123, 387–411.CrossRefGoogle Scholar
Dilek, Y and Furnes, H (2014) Ophiolites and their origins. Elements 10, 93–100.CrossRefGoogle Scholar
Ding, JX, Han, CM, Xiao, WJ, Wang, ZM and Yang, XM (2015) Geochemistry and U–Pb geochronology of tungsten deposit of Huaniushan island arc in the Beishan Orogenic Belt, and its geodynamic background. Acta Petrologica Sinica 31, 594–616 (in Chinese with English abstract).Google Scholar
Elliott, T, Plank, T, Zindler, A, White, W and Bourdon, B (1997) Element transport from slab to volcanic front at the Mariana arc. Journal of Geophysical Research: Solid Earth 102, 14991–5019.CrossRefGoogle Scholar
Fliedner, M and Klemperer, S (2000) Crustal structure transition from oceanic arc to continental arc, Eastern Aleutian Islands and Alaska Peninsula. Earth and Planetary Science Letters 179, 567–79.CrossRefGoogle Scholar
Gangu Survey Insitute (2001) Geological Map of the Mazongshan Region, China, 1:250,000. No. 3 Geological Survey Team of the Gansu Bureau of Geology and Mineral Deposits (in Chinese).Google Scholar
Gangu Survey Insitute (2008) Geological Map of the Mazongshan Region, China, 1:50,000. No. 3 Geological Survey Team of the Gansu Bureau of Geology and Mineral Deposits (in Chinese).Google Scholar
Guo, QQ, Xiao, WJ, Hou, QL, Windley, BF, Han, CM, Tian, ZH and Song, DF (2014) Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt. Lithos 184–187, 361–78.CrossRefGoogle Scholar
He, ZY, Zhang, ZM, Zong, KQ, Xiang, H, Chen, XJ and Xia, MJ (2014a) Zircon U–Pb and Hf isotopic studies of the Xingxingxia Complex from Eastern Tianshan (NW China): significance to the reconstruction and tectonics of the southern Central Asian Orogenic Belt. Lithos 190–191, 485–99.CrossRefGoogle Scholar
He, ZY, Zhang, ZM, Zong, KQ, Xiang, H and Klemd, R (2014b) Metamorphic P–T–t evolution of mafic HP granulites in the northeastern segment of the Tarim Craton (Dunhuang block): evidence for early Paleozoic continental subduction. Lithos 196–197, 1–13.CrossRefGoogle Scholar
Hou, QY, Wang, Z, Liu, JB, Wang, J and Li, DP (2012) Geochemistry characteristics and SHRIMP dating of Yueyashan ophiolite in Beishan orogen. Geoscience 26, 1008–18 (in Chinese with English abstract).Google Scholar
Hu, XZ, Zhao, GC, Hu, XY, Liao, YF and Cheng, HF (2015) Geological characteristics, formation epoch and geotectonic significance of the Yueyashan ophiolitic tectonic mélange in the Beishan area, Inner Mongolia. Geological Bulletin of China 34, 425–36 (in Chinese with English abstract).Google Scholar
Isozaki, Y (1996) Anatomy and genesis of a subduction-related orogen: a new view of geotectonic subdivision and evolution of the Japanese Islands. Island Arc 5, 289–320.CrossRefGoogle Scholar
Jahn, B-M, Wu, F 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
Kröner, A, Hegner, E, Lehmann, B, Heinhorst, J, Wingate, MTD, Liu, DY and Ermelov, P (2008) Palaeozoic arc magmatism in the Central Asian Orogenic Belt of Kazakhstan: SHRIMP zircon ages and whole-rock Nd isotopic systematics. Journal of Asian Earth Sciences 32, 118–30.CrossRefGoogle Scholar
Kusky, TM, Windley, BF, Safonova, I, Wakita, K, Wakabayashi, J, Polat, A and Santosh, M (2013) Recognition of ocean plate stratigraphy in accretionary orogens through Earth history: a record of 3.8 billion years of sea floor spreading, subduction, and accretion. Gondwana Research 24, 501–47.CrossRefGoogle Scholar
Li, XM, Yu, JY, Wang, GQ and Wu, P (2012) Geochronology of Jijitaizi ophiolite in Beishan area, Gansu Province, and its geological significance. Geological Bulletin of China 31, 2025–31 (in Chinese with English abstract).Google Scholar
Liu, YS, Hu, ZC, Gao, S, Günther, 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
Ludwig, KR (2000) Users Manual for Isoplot/Ex: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Berkeley, Special Publication 1a, 53.Google Scholar
Mao, QG, Xiao, WJ, Fang, TH, Wang, JB, Han, CM, Sun, M and Yuan, C (2012) Late Ordovician to early Devonian adakites and Nb-enriched basalts in the Liuyuan area, Beishan, NW China: implications for early Paleozoic slab-melting and crustal growth in the southern Altaids. Gondwana Research 22, 534–53.CrossRefGoogle Scholar
Mao, QG, Xiao, WJ, Windley, BF, Han, CM, Qu, JF, Ao, SJ, Zhang, JE and Guo, QQ (2011) The Liuyuan complex in the Beishan, NW China: a Carboniferous–Permian ophiolitic fore-arc sliver in the southern Altaids. Geological Magazine 149, 483–506.CrossRefGoogle Scholar
Maruyama, S (1997) Pacific-type orogeny revisited: Miyashiro-type orogeny proposed. Island Arc 6, 91–120.CrossRefGoogle Scholar
Pearce, JA (2008) Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust. Lithos 100, 14–48.CrossRefGoogle Scholar
Pearce, JA (2014) Geochemical fingerprinting of the Earthʼs oldest rocks. Geology 42, 175–76.CrossRefGoogle Scholar
Reagan, MK, Ishizuka, O, Stern, RJ, Kelley, KA, Ohara, Y, Blichert-Toft, J, Bloomer, SH, Cash, J, Fryer, P, Hanan, BB, Hickey-Vargas, R, Ishii, T, Kimura, J-I, Peate, DW, Rowe, MC and Woods, M (2010) Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system. Geochemistry, Geophysics, Geosystems 11, published online 6 March 2010, doi: 10.1029/2009GC002871.CrossRefGoogle Scholar
Ren, BC, He, SP, Yao, WG and Fu, LP (2001) Rb-Sr isotope age Niujuanzi ophiolite and its tectonic significance in Beishan district, Gansu. Northwestern Geology 34, 21–7 (in Chinese with English abstract).Google Scholar
Safonova, IY, Perfilova, AA, Obut, OT, Savinsky, IA, Chyornyi, RI, Petrenko, NA, Gurova, AV, Kotler, PD, Khromykh, SV, Krivonogov, SK and Maruyama, S (2019) The Itmurundy accretionary complex, Northern Balkhash area: geological structure, stratigraphy and tectonic origin. Russian Journal of Pacific Geology 13, 283–96.CrossRefGoogle Scholar
Safonova, IY and Santosh, M (2014) Accretionary complexes in the Asia-Pacific region: tracing archives of ocean plate stratigraphy and tracking mantle plumes. Gondwana Research 25, 126–58.CrossRefGoogle Scholar
Safonova, IY, Seltmann, R, Kröner, A, Gladkochub, D, Kim, J-Y, Schulmann, K, Xiao, W, Komiya, T and Sun, M (2011) A new concept of continental construction in the Central Asian Orogenic Belt: (compared to actualistic examples from the Western Pacific). Episodes 34, 1–10.CrossRefGoogle Scholar
Schulmann, K and Paterson, S (2011) Geodynamics of Asian continental growth. Nature Geoscience 4, 827–29.CrossRefGoogle Scholar
Şengör, AMC, Natal’in, BA and Burtman, VS (1993) Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia. Nature 364, 299–307.CrossRefGoogle Scholar
Şengör, AMC, Natal’in, BA, Sunal, G and Voo, RVD (2014) A new look at the Altaids: a super-orogenic complex in northern and central Asia as a factory of continental crust. Part I: geological data compilation (exclusive of palaeomagnetic observations). Austrian Journal of Earth Sciences 107, 169–232.Google Scholar
Shervais, JW (1982) Ti-V plots and the petrogenesis of modern and ophiolitic lavas. Earth and Planetary Science Letters 59, 101–18.CrossRefGoogle Scholar
Shervais, JW (2001) Birth, death, and resurrection: The life cycle of suprasubduction zone ophiolites. Geochemistry, Geophysics, Geosystems 2, 2000GC000080.CrossRefGoogle Scholar
Shi, YR, Zhang, W, Kröner, A, Li, LL and Jian, P (2018) Cambrian ophiolite complexes in the Beishan area, China, southern margin of the Central Asian Orogenic Belt. Journal of Asian Earth Sciences 153, 193–205.CrossRefGoogle Scholar
Shu, LS, Wang, B and Zhu, WB (2007) Age of radiolarian fossils from the Heiyingshan Ophiolitic Mélange, Southern Tianshan Belt, NW China, and its tectonic significance. Acta Geologica Sinica 81, 1161–70.Google Scholar
Song, DF, Xiao, WJ, Han, CM, Li, JL, Qu, JF, Guo, QQ, Lin, LN and Wang, ZM (2013a) Progressive accretionary tectonics of the Beishan orogenic collage, southern Altaids: insights from zircon U–Pb and Hf isotopic data of high-grade complexes. Precambrian Research 227, 368–88.CrossRefGoogle Scholar
Song, DF, Xiao, WJ, Han, CM and Tian, ZH (2013b) Geochronological and geochemical study of gneiss–schist complexes and associated granitoids, Beishan Orogen, southern Altaids. International Geology Review 55, 1705–27.CrossRefGoogle Scholar
Song, DF, Xiao, WJ, Han, CM and Tian, ZH (2014) Polyphase deformation of a Paleozoic forearc–arc complex in the Beishan orogen, NW China. Tectonophysics 632, 224–43.CrossRefGoogle Scholar
Song, DF, Xiao, WJ, Han, CM, Tian, ZH and Wang, ZM (2013c) Provenance of metasedimentary rocks from the Beishan orogenic collage, southern Altaids: constraints from detrital zircon U–Pb and Hf isotopic data. Gondwana Research 24, 1127–51.CrossRefGoogle Scholar
Song, DF, Xiao, WJ, Windley, BF, Han, CM and Tian, ZH (2015) A Paleozoic Japan-type subduction-accretion system in the Beishan orogenic collage, southern Central Asian Orogenic Belt. Lithos 224–225, 195–213.CrossRefGoogle Scholar
Stolz, AJ, Jochum, KP, Spettel, B and Hofmann, AW (1996) Fluid- and melt-related enrichment in the sub-arc mantle: Evidence from Nb/Ta variations in island-arc basalts. Geology 24, 586–90.2.3.CO;2>CrossRefGoogle Scholar
Sun, S-S and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and source processes. In Magamtism in the Ocean Basins (eds Saunders, AD and Norry, MJ), pp. 313–45. Geological Society of London, Special Publication no. 42.Google Scholar
Tian, ZH, Xiao, WJ, Windley, BF, Lin, LN, Han, CM, Zhang, JE, Wan, B, Ao, SJ, Song, DF and Feng, JY (2014) Structure, age, and tectonic development of the Huoshishan–Niujuanzi ophiolitic mélange, Beishan, southernmost Altaids. Gondwana Research 25, 820–41.Google Scholar
Tian, ZH, Xiao, WJ, Windley, BF, Zhang, JE, Zhang, ZY and Song, DF (2016) Carboniferous rifted arcs leading to an archipelago of multiple arcs in the Beishan–Tianshan orogenic collages (NW China). International Journal of Earth Sciences 106, 2319–42.CrossRefGoogle Scholar
Wakabayashi, J (2011) Mélanges of the Franciscan Complex, California: Diverse structural settings, evidence for sedimentary mixing, and their connection to subduction processes. In Mélanges: Processes of Formation and Societal Significance (eds Wakabayashi, J and Dilek, Y), pp. 117–41. Geological Society of America, Boulder, Special Paper no. 480.CrossRefGoogle Scholar
Wakita, K, Pubellier, M and Windley, B (2013) Tectonic processes, from rifting to collision via subduction, in SE Asia and the western Pacific: a key to understanding the architecture of the Central Asian Orogenic Belt. Lithosphere 5, 265–76.CrossRefGoogle Scholar
Wan, TF and Zhu, H (2011) Chinese continental blocks in global Paleocontinental reconstruction during Paleozoic and Mesozoic. Acta Geologica Sinica (English Edition) 85, 581–97.CrossRefGoogle Scholar
Wang, GQ, Li, XM, Xu, XY and Wu, P (2014) Zircon U–Pb chronological study of the Hongshishan ophiolite in the Beishan area and their tectonic significance. Acta Petrologica Sinica 30, 1685–94 (in Chinese with English abstract).Google Scholar
Wang, GQ, Li, XM, Xu, XY, Yu, JY, Guo, L, Yan, QJ, Ji, B and Wu, P (2016) Geochemistry of Gongpoquan Group in the Beishan area, Gansu Province: constraints on petrogenesis and tectonic setting. Acta Geologica Sinica 90, 2603–19.Google Scholar
Wang, SD, Zhang, KX, Song, BW, Li, SC, Li, JX, Yu, JY and Bu, JJ (2018a) Detrital Zircon U-Pb geochronology from greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: provenance and tectonic implications. Journal of Earth Science 29, 103–13.Google Scholar
Wang, SD, Zhang, KX, Song, BW, Li, SC, Li, M and Zhou, J (2017) Geochronology and geochemistry of the Niujuanzi ophiolitic mélange, Gansu Province, NW China: implications for tectonic evolution of the Beishan Orogenic Collage. International Journal of Earth Sciences 107, 269–89.CrossRefGoogle Scholar
Wang, XY, Yuan, C, Zhang, YY, Long, XP, Sun, M, Wang, LX, Soldner, J and Lin, ZF (2018b) S-type granite from the Gongpoquan arc in the Beishan Orogenic Collage, southern Altaids: implications for the tectonic transition. Journal of Asian Earth Sciences 153, 206–22.CrossRefGoogle Scholar
Wilhem, C, Windley, BF and Stampfli, GM (2012) The Altaids of Central Asia: a tectonic and evolutionary innovative review. Earth-Science Reviews 113, 303–41.CrossRefGoogle Scholar
Winchester, JA and Floyd, PA (1977) Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology 20, 325–43.CrossRefGoogle Scholar
Windley, B and Xiao, WJ (2018) Ridge subduction and slab windows in the Central Asian Orogenic Belt: tectonic implications for the evolution of an accretionary orogen. Gondwana Research 61, 73–87.CrossRefGoogle Scholar
Windley, BF (1992) Proterozoic collisional and accretionary orogens. In Proterozoic Crustal Evolution (ed. Condie, KC), pp. 419–46. Elsevier: Amsterdam.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
Wood, DA (1980) The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification. Earth and Planetary Science Letters 50, 1–30.CrossRefGoogle Scholar
Wu, P, Wang, GQ, Li, XM, Yu, JY and Kang, L (2012) The age of Niujuanzi ophiolite in Beishan area of Gansu Province and its geological significance. Geological Bulletin of China 31, 2032–37 (in Chinese with English abstract).Google Scholar
Xiao, QH, Li, TD, Pan, GT, Lu, SN, Ding, XZ, Deng, JF, Feng, YM, Liu, Y, Kou, CH and Yang, LL (2016) Petrologic ideas for identification of ocean-continent transition: recognition of intra-oceanic arc and initial subduction. Geology in China 43, 721–37 (in Chinese with English abstract).Google Scholar
Xiao, WJ, Han, CM, Liu, W, Wan, B, Zhang, JE, Ao, SJ, Zhang, ZY, Song, DF, Tian, ZH and Luo, J (2014) How many sutures in the southern Central Asian Orogenic Belt: insights from East Xinjiang–West Gansu (NW China)? Geoscience Frontiers 5, 525–36.CrossRefGoogle Scholar
Xiao, WJ, Han, CM, Yuan, C, Sun, M, Zhao, GC and Shan, YH (2010a) Transitions among Mariana-, Japan-, Cordillera- and Alaska-type arc systems and their final juxtapositions leading to accretionary and collisional orogenesis. In The Evolving Continents: Understanding Processes of Continental Growth (eds TM Kusky, M-G Zhai and W Xiao), pp. 35–53. Geological Society of London, Special Publication no. 338.CrossRefGoogle Scholar
Xiao, WJ, Huang, BC, Han, CM, Sun, S and Li, JL (2010b) A review of the western part of the Altaids: a key to understanding the architecture of accretionary orogens. Gondwana Research 18, 253–73.CrossRefGoogle Scholar
Xiao, WJ, Mao, QG, Windley, BF, Han, CM, Qu, JF, Zhang, JE, Ao, SJ, Guo, QQ, Cleven, NR, Lin, SF, Shan, YH and Li, JL (2010c) Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage. American Journal of Science 310, 1553–94.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Badarch, G, Sun, S, Li, JL, Qin, KZ and Wang, ZH (2004) Palaeozoic accretionary and convergent tectonics of the southern Altaids: implications for the growth of Central Asia. Journal of the Geological Society, London 161, 339–42.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Hao, J and Zhai, MG (2003) Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: termination of the central Asian orogenic belt. Tectonics 22, 1–15.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Sun, S, Li, JL, Huang, BC, Han, CM, Yuan, C, Sun, M and Chen, HL (2015) A tale of amalgamation of three Permo-Triassic collage systems in Central Asia: oroclines, sutures, and terminal accretion. Annual Review of Earth and Planetary Sciences 43, 477–507.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Yuan, C, Sun, M, Han, CM, Lin, SF, Chen, HL, Yan, QR, Liu, DY, Qin, KZ, Li, JL and Sun, S (2009) Paleozoic multiple subduction-accretion process of the southern Altaids. American Journal of Science 309, 221–70.CrossRefGoogle Scholar
Yu, FS, Li, JB and Wang, T (2006) The U-Pb isotopic age of zircon from Hongliuhe ophiolites in East Tianshan mountains, Northwest China. Acta Geoscientica Sinica 27, 213–16 (in Chinese with English abstract).Google Scholar
Zhang, KX, Feng, QL, Song, BW, Zhang, ZY, Wang, YH, Pan, GT, Lu, SN, Zhao, XM and Xing, GF (2014a) Non-Smithian strata in the orogen. Earth Science Frontiers (China University of Geosciences (Beijing); Peking University) 21, 36–47 (in Chinese with English abstract).Google Scholar
Zhang, YY and Guo, ZJ (2008) Accurate constraint on formation and emplacement age of Hongliuhe ophiolite, boundary region between Xinjiang and Gansu Provinces and its tectonic implications. Acta Petrologica Sinica 24, 803–9 (in Chinese with English abstract).Google Scholar
Zhang, KX, He, WH, Xu, YD, Luo, MS, Song, BW, Kou, XH and Xing, ZY (2018) Explanatory Note of the Sedimentary Tectonic Map of China (1:2 500 000). Beijing, China: Geological Publishing House.Google Scholar
Zhang, KX, He, WH, Xu, YD, Luo, MS, Song, BW, Kou, XH, Zhang, ZY, Xiao, QH and Pan, GT (2016) Palaeogeographic distribution and tectonic evolution of OPS in China. Earth Science Frontiers (China University of Geosciences (Beijing); Peking University) 23, 24–30 (in Chinese with English abstract).Google Scholar
Zhang, KX, He, WH, Xu, YD, Luo, MS, Song, BW, Zhang, ZY, Pan, GT, Wang, YH, Zhao, XM and Xing, GF (2014b) Subdivision and identification of sedimentary tectonic facies. Earth Science—Journal of China University of Geosciences 39, 915–28 (in Chinese with English abstract).Google Scholar
Zhang, KX, Pan, GT, He, WH, Xiao, QH, Xu, Y-D, Zhang, Z, Lu, S, Deng, J, Feng, Y, Li, J, Zhao, X, Xing, G, Wang, Y, Yin, F, Hao, G, Zhang, C, Zhang, J and Gong, Y (2015) New division of tectonic-strata super-region in China. Earth Science—Journal of China University of Geosciences 40, 206–33 (in Chinese with English abstract).Google Scholar
Zheng, RG, Li, JY and Xiao, WJ (2019) Mid-Paleozoic ridge subduction in the Central Beishan of the southern Altaids: evidence from geochemical, Sr–Nd and zircon U–Pb–Hf–O isotopic data of Gongpoquan volcanic rocks. Journal of the Geological Society, London 176, 755–70.CrossRefGoogle Scholar
Zheng, RG, Wu, TR, Zhang, W, Xu, C and Meng, QP (2013) Late Paleozoic subduction system in the southern Central Asian Orogenic Belt: evidences from geochronology and geochemistry of the Xiaohuangshan ophiolite in the Beishan orogenic belt. Journal of Asian Earth Sciences 62, 463–75.CrossRefGoogle Scholar
Zheng, RG, Xiao, WJ, Li, JY, Wu, TR and Zhang, W (2018) A Silurian-early Devonian slab window in the southern Central Asian Orogenic Belt: evidence from high-Mg diorites, adakites and granitoids in the western Central Beishan region, NW China. Journal of Asian Earth Sciences 153, 75–99.CrossRefGoogle Scholar
Zheng, YF (2012) Metamorphic chemical geodynamics in continental subduction zones. Chemical Geology 328, 5–48.CrossRefGoogle Scholar
Zheng, YF (2019) Subduction zone geochemistry. Geoscience Frontiers 10, 1223–54.CrossRefGoogle Scholar
Zuo, GC, Jin, SQ and Feng, TQ (1994) Conodonts were found in the Gansu Province. Regional Geology of China 2, 185 (in Chinese with English abstract).Google Scholar
Zuo, GC, Liu, YK and Liu, CY (2003) Framework and evolution of the tectonic structure in Beishan area across Gansu Province, Xinjiang Autonomous region and Inner Mongolia Autonomous region. Acta Geologica Gansu 12, 1–15 (in Chinese with English abstract).Google Scholar