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Petrogenesis and tectonic setting of Late Devonian high-Mg andesites in the Beishan orogen, NW China

Published online by Cambridge University Press:  06 December 2021

Guo-Qiang Wang Open the ORCID record for Guo-Qiang Wang [Opens in a new window] ,
Xiang-Min Li ,
Ji-Yuan Yu ,
Tao Bu ,
Bo-Tao Huang  and
Yu-Jie Liu
Guo-Qiang Wang*
Affiliation:
Xi’an Center of China Geological Survey, Xi’an, 710054, Shaanxi, China Centre for Orogenic Belt Geology, China Geological Survey, Xi’an, 710054, Shaanxi, China Northwest China Center for Geoscience Innovation, Xi’an, 710054, Shaanxi, China
Xiang-Min Li
Affiliation:
Xi’an Center of China Geological Survey, Xi’an, 710054, Shaanxi, China Centre for Orogenic Belt Geology, China Geological Survey, Xi’an, 710054, Shaanxi, China Northwest China Center for Geoscience Innovation, Xi’an, 710054, Shaanxi, China
Ji-Yuan Yu
Affiliation:
Xi’an Center of China Geological Survey, Xi’an, 710054, Shaanxi, China Centre for Orogenic Belt Geology, China Geological Survey, Xi’an, 710054, Shaanxi, China Northwest China Center for Geoscience Innovation, Xi’an, 710054, Shaanxi, China
Tao Bu
Affiliation:
Xi’an Center of China Geological Survey, Xi’an, 710054, Shaanxi, China
Bo-Tao Huang
Affiliation:
Xi’an Center of China Geological Survey, Xi’an, 710054, Shaanxi, China
Yu-Jie Liu
Affiliation:
Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, 710061, Shaanxi, China
*
Author for correspondence: Guo-Qiang Wang, Email: [email protected]
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Abstract

High-Mg andesites (HMAs) are crucial for the reconstruction of plate tectonics, continental margin formation and lithospheric evolution. In this study, we present new fossil age, whole-rock geochemical and Sr–Nd isotope data on the newly discovered Dundunshan Group HMAs in the Dundunshan area of the Beishan orogen (central-southern Central Asian Orogenic Belt). The Dundunshan HMA samples are characterized by high MgO (6.47–7.02 wt%) contents and high Mg# values (67.27–68.77), with SiO2 (58.57–62.13 wt%), Al2O3 (14.49–16.07 wt%) and CaO (5.05–6.24 wt%) resembling typical HMAs. The Dundunshan HMA samples are calc-alkaline and strongly enriched in light rare earth elements (LREEs) and large-ion lithophile elements (LILEs), with slightly negative Eu anomaly and high-field-strength element (HFSE) depletions. Their (87Sr/86Sr)i ratios (0.7041–0.7057) and ϵNd(t) (3.73–5.59) indicate that the Dundunshan HMAs were mainly formed by the interactions between subducted oceanic sediment-derived melts and mantle peridotites. Fossil evidence and published radiometric age data constrain the formation of the Dundunshan HMAs to early Late Devonian time. Sedimentological features of the Middle Devonian Sangejing Formation and regional tectonic correlation suggest that the Hongliuhe–Niujuanzi–Xichangjing Ocean in the Dundunshan area was likely closed during late Middle Devonian time, and that the Dundunshan HMAs were formed in a post-collision extensional setting.

Keywords

high-Mg andesitesgeochemistrypetrogenesistectonic settingLate DevonianBeishanCentral Asian Orogenic Belt
Type
Original Article
Information
Geological Magazine , Volume 159 , Issue 4 , April 2022 , pp. 577 - 592
Copyright
© The Author(s), 2021. Published by Cambridge University Press

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References

Aldanmaz, E, Pearce, JA, Thirlwall, MF and Mitchell, JG (2000) Petrogenetic evolution of late Cenozoic, post-collision volcanism in western Anatolia, Turkey. Journal of Volcanology & Geothermal Research 102, 67–95.CrossRefGoogle Scholar
Allen, MB, Windley, BF and Zhang, Z (1992) Paleozoic collisional tectonics and magmatism of the Chinese Tien Shan, Central Asia. Tectonophysics 220, 89–115.CrossRefGoogle Scholar
Ao, SJ, Xiao, WJ, Windley, BF, Mao, QG, Han, CM, Zhang, JE, Yang, L and Geng, J (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
BGMRG (No.1 team, Bureau of Geology and Mineral Resources of Gansu Province) (1967) Anbei sheet map, scale 1:200000 (in Chinese). Lan Zhou: Gansu Geological Bureau.Google Scholar
Bloomer, SH and Hawkins, JW (1987) Petrology and geochemistry of boninite series volcanic rocks from the Mariana trench. Contributions to Mineralogy and Petrology 97, 361–77.CrossRefGoogle Scholar
Brookfield, ME (2000) Geological development and Phanerozoic crustal accretion in the western segment of the southern Tien Shan (Kyrgyzstan, Uzbekistan and Tajikistan). Tectonophysics 328, 1–14.CrossRefGoogle Scholar
Cameron, WE, Nisbet, EG and Dietrich, VJ (1979) Boninites, komatiites and ophiolitic basalts. Nature 280, 550–3.CrossRefGoogle Scholar
Chen, C, Lu, H, Jia, D, Cai, D and Wu, S (1999) Closing history of the southern Tianshan oceanic basin, western China: an oblique collisional orogeny. Tectonophysics 302, 23–40.CrossRefGoogle Scholar
Dai, S, Fang, XM, Zhang, X, Wang, FC, Ren, YZ, Gao, ZK, Lei, TZ and Cheng, Y (2003) Island arc north of the Tarim-SK plate: the geology and geochemistry of Gongpoquan Group. Journal of Lanzhou University (Natural Science) 39, 80–7 (in Chinese with English abstract).Google Scholar
Dai, S, Ren, YZ, Chen, Y, Gao, ZK, Zhang, X and Wang, FC (2002) The ore-bearing porphyry at island-arc in the Gongpoquan Copper deposit: its geology and geochemistry. Journal of Lanzhou University (Natural Science) 38, 100–7 (in Chinese with English abstract).Google Scholar
Defant, MJ and Drummond, MS (1990) Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature 347, 662–5.CrossRefGoogle Scholar
Deniel, C and Pin, C (2001) Single-stage method for the simultaneous isolation of lead and strontium from silicate samples for isotopic measurements. Analytica Chimica Acta 426, 95–103.CrossRefGoogle Scholar
Dong, YP, Zhang, GW, Neubauer, F, Liu, X, Hauzenberger, C, Zhou, D and Li, W (2011) Syn- and post-collisional granitoids in the Central Tianshan orogen: geochemistry, geochronology and implications for tectonic evolution. Gondwana Research 20, 568–81.CrossRefGoogle Scholar
Gan, C, Wang, Y, Barry, TL, Zhang, Y and Qian, X (2020) Late Jurassic high-Mg andesites in the Youjiang Basin and their significance for the southward continuation of the Jiangnan Orogen, South China. Gondwana Research 77, 260–73.CrossRefGoogle Scholar
Gao, J and Klemd, R (2003) Formation of HP–LT rocks and their tectonic implications in the western Tianshan Orogen, NW China: geochemical and age constraints. Lithos 66, 1–22.CrossRefGoogle Scholar
Gao, J, Klemd, R, Qian, Q, Zhang, X and Li, J (2011) The collision between the Yili and Tarim blocks of the Southwestern Altaids: geochemical and age constraints of a leucogranite dike crosscutting the HP–LT metamorphic belt in the Chinese Tianshan Orogen. Tectonophysics 499, 118–31.CrossRefGoogle Scholar
Gao, S, Rudnick, RL, Yuan, HL, Liu, XM, Liu, YS, Xu, WL, Ling, WL, John, A, Wang, XC and Wang, QH (2004) Recycling lower continental crust in the North China craton. Nature 432, 892–7.CrossRefGoogle ScholarPubMed
Glorie, S, Grave, JD, Buslov, MM, Elburg, MA, Stockli, DF, Gerdes, A and Haute, PVD (2010) Multi-method chronometric constraints on the evolution of the Northern Kyrgyz Tien Shan granitoids (Central Asian Orogenic Belt): from emplacement to exhumation. Journal of Asian Earth Sciences 38, 131–46.CrossRefGoogle Scholar
Guo, QQ, Chung, SL, Xiao, WJ, Hou, QL and Li, S (2017) Petrogenesis and tectonic implications of Late Devonian arc volcanic rocks in southern Beishan orogen, NW China: geochemical and Nd–Sr–Hf isotopic constraints. Lithos 278–281, 84–96.CrossRefGoogle 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
Han, BF, Ji, JQ, Song, B, Chen, LH and Li, ZH (2004) Zircon U-Pb dating of the mafic-ultramafic complex related to the Cu-Ni sulfide deposit and its geological significance in the Kalatongke and Huangshandong, Xinjiang, China. China Science Bulletin 49, 2324–8 (in Chinese with English abstract).Google Scholar
Han, BF, Wang, SG, Jahn, BM, Hong, DW, Kagami, H and Sun, YL (1997) Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd-Sr isotopic evidence, and implications for Phanerozoic crustal growth. Chemical Geology 138, 135–59.CrossRefGoogle Scholar
Hanyu, T, Tatsumi, Y and Nakai, SI (2002) A contribution of slab-melts to the formation of high-Mg andesite magmas; Hf isotopic evidence from SW Japan. Geophysical Research Letters 29, 81–4.CrossRefGoogle Scholar
He, SP, Zhou, HW, Ren, BC, Yao, WG and Fu, LP (2005) Crustal evolution of Palaeozoic in Beishan area, Gansu and Inner Mongolia, China. Northwestern Geology 38, 6–15 (in Chinese with English abstract).Google Scholar
He, SP, Zhou, HW, Yao, WG, Ren, BC and Fu, LP (2004) Discovery and significance of radiolarian from Middle Devonian conglomerate in Beishan area, Gansu. Northwestern Geology 37, 24–8 (in Chinese with English abstract).Google Scholar
Hirose, Kei (1997) Melting experiments on lherzolite KLB-1 under hydrous conditions and generation of high-magnesian andesitic melts. Geology 25, 42–4.2.3.CO;2>CrossRefGoogle Scholar
Jahn, B (2004) Phanerozoic continental growth in Central Asia. Journal of Asian Earth Sciences 23, 599–603.CrossRefGoogle Scholar
Jahn, B, Wu, F and Chen, B (2000) Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic. Episodes 23, 82–92.CrossRefGoogle Scholar
JBGMRG (Jiuquan team, Bureau of Geology and Mineral Resources of Gansu Province) (1995) Sangejing sheet map, scale 1:50000 (in Chinese with English abstract). Lan Zhou: Gansu Geological Bureau.Google Scholar
JBGMRG (Jiuquan team, Bureau of Geology and Mineral Resources of Gansu Province) (1998) Gangliu sheet map, scale 1:50000 (in Chinese with English abstract). Lan Zhou: Gansu Geological Bureau.Google Scholar
Kay, RW (1978) Aleutian magnesian andesites: melts from subducted Pacific ocean crust. Journal of Volcanology & Geothermal Research 4, 117–32.CrossRefGoogle Scholar
Kay, RW, Mahlburgkay, S, Stoeckhert, B and Wedepohl, KH (1991) Creation and destruction of lower continental crust. Geologische Rundschau 80, 259–78.CrossRefGoogle Scholar
Kay, SM, Ramos, VA and Marquez, M (1993) Evidence in Cerro Pampa volcanic rocks for slab-melting prior to ridge-trench collision in Southern South America. Journal of Geology 101, 703–14.CrossRefGoogle Scholar
Kelemen, PB (1995) Genesis of high Mg# andesites and the continental crust. Contributions to Mineralogy and Petrology 120, 1–19.CrossRefGoogle Scholar
Kelemen, PB, Hart, SR and Bernstein, S (1998) Silica enrichment in the continental upper mantle via melt/rock reaction. Earth & Planetary Science Letters 164, 387–406.CrossRefGoogle Scholar
Khanna, TC, Sai, VVS, Bizimis, M and Krishna, AK (2015) Petrogenesis of basalt–high-Mg andesite–adakite in the Neoarchean Veligallu Greenstone Terrane: geochemical evidence for a rifted back-arc crust in the eastern Dharwar craton, India. Precambrian Research 258, 260–77.CrossRefGoogle Scholar
Klemd, R, Bröcker, M, Hacker, B, Gao, J, Gans, P and Wemmer, K (2005) New age constraints on the metamorphic evolution of the high-pressure/low-temperature belt in the western Tianshan Mountains, NW China. Journal of Geology 113, 157–68.CrossRefGoogle Scholar
Konopelko, D, Biske, G, Seltmann, R, Eklund, O and Belyatsky, B (2007) Hercynian post-collisional A-type granites of the Kokshaal Range, Southern Tien Shan, Kyrgyzstan. Lithos 97, 140–60.CrossRefGoogle Scholar
Konopelko, D, Seltmann, R, Biske, G, Lepekhina, E and Sergeev, S (2009) Possible source dichotomy of contemporaneous post-collisional barren I-type versus tin-bearing A-type granites, lying on opposite sides of the South Tien Shan suture. Ore Geology Reviews 35, 206–16.CrossRefGoogle Scholar
Lassiter, JC and Depaolo, DJ (1997) Plumers/lithosphere interaction in the generation of contimental and oceanic flood basalts: chemical and isotope constraints. In: Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism (eds Mahoney, JJ and Coffin, MF), pp. 335–55. Washington: American Geophysical Union, Geophysical Monograph Series, no. 100.Google Scholar
Le Bas, MJ (2000) IUGS reclassification of the high-Mg and picritic volcanic rocks. Journal of Petrology 41, 1467–70.CrossRefGoogle Scholar
Le Maitre, RW, Bateman, P, Dudek, A, Keller, J, Lameyre, P, Le Bas, MJ, Sabine, PA, Schmid, R, Sorensen, H, Streekeisen, A, Wolley, AR and Zanettin, B (1989) A Classification and Glossary of Terms: Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks. Oxford, Blackwell.Google Scholar
Li, QL, Lin, W, Su, W, Li, XH, Shi, YH, Liu, Y and Tang, GQ (2011a) SIMS U–Pb rutile age of low-temperature eclogites from southwestern Chinese Tianshan, NW China. Lithos 122, 76–86.CrossRefGoogle Scholar
Li, S, Wang, T, Tong, Y, Hong, DW and Ouyang, ZX (2009) Identification of the Early Devonian Shuangfengshan A-type granites in Liuyuan area of Beishan and its implications to tectonic evolution. Acta Petrologica et Mineralogica 28, 407–21 (in Chinese with English abstract).Google Scholar
Li, S, Wang, T, Tong, Y, Wang, YB, Hong, DW and Auyang, ZX (2011b) Zircon U-Pb age, origin and its tectonic significances of Huitongshan Devonian K-feldspar granites from Beishan orogen, NW China. Acta Petrologica Sinica 27, 3055–70 (in Chinese with English abstract).Google Scholar
Li, WP, Wang, T, Li, JB, Kang, X, Yu, FS, Han, QJ and Ma, ZP (2001) The U-Pb age of zircon from Late Caledonian granitoids in Hongliuhe area, east Tianshan mountains, northwest China and its geological implications. Acta Geoscientia Sinica 22, 231–5 (in Chinese with English abstract).Google Scholar
Li, XM, Yu, JY, Wang, GQ, Wu, P and Zhou, ZQ (2011c) LA-ICP-MS zircon U-Pb dating of Devonian Sangejing Formation and Dundunshan Group in Hongliuyuan, Beishan area, Gansu Province. Geological Bulletin of China 30, 1501–7 (in Chinese with English abstract).Google Scholar
Li, YJ, Xu, Q, Yang, GX, Zhao, WD and Liu, J (2016) Intracontinental “lagged arc volcanic rocks” and its geological significance: evidence from early Permian lagged arc magmatism in northern Urho area of Western Junggar. Earth Science Frontiers 23, 190–9 (in Chinese with English abstract).Google Scholar
Liao, WH (2001) Query the validity of the “South-type” Devonian of the Hongliuyuan area, Gansu. Journal of Stratigraphy 25, 121–2 (in Chinese with English abstract).Google Scholar
Liu, X, Chen, B, Jahn, B, Wu, G and Liu, Y (2011) Early Paleozoic (ca. 465 Ma) eclogites from Beishan (NW China) and their bearing on the tectonic evolution of the southern Central Asian Orogenic Belt. Journal of Asian Earth Sciences 42, 715–31.Google 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
Míková, J and Denková, P (2007) Modified chromatographic separation scheme for Sr and Nd isotope analysis in geological silicate samples. Journal of Geosciences 52, 221–6.Google Scholar
Niu, YZ, Liu, CY, Shi, GR, Lu, JC, Xu, W and Shi, JZ (2018) Unconformity-bounded Upper Paleozoic megasequences in the Beishan Region (NW China) and implications for the timing of the Paleo-Asian Ocean closure. Journal of Asian Earth Sciences 167, 11–32.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
Pin, C and Zalduegui, JS (1997) Sequential separation of light rare-earth elements, thorium and uranium by miniaturized extraction chromatography: application to isotopic analyses of silicate rocks. Analytica Chimica Acta 339, 79–89.CrossRefGoogle Scholar
Plank, T, Langmuir, CH, Albarede, F, Blicherttoft, J, Staudigel, H and White, WM (1998) The chemical composition of subducting sediment and its consequences for the crust and mantle. Chemical Geology 145, 325–94.CrossRefGoogle Scholar
Rapp, RP, Shimizu, N, Norman, MD and Applegate, GS (1999) Reaction between slab-derived melts and peridotite in the mantle wedge: experimental constraints at 3.8 GPa. Chemical Geology 160, 335–56.CrossRefGoogle Scholar
Rogers, G, Saunders, AD, Terrell, DJ, Verma, SP and Marriner, GF (1985) Geochemistry of Holocene volcanic rocks associated with ridge subduction in Baja California, Mexico. Nature 315, 389–92.CrossRefGoogle Scholar
Saunders, AD, Rogers, G, Marriner, GF, Terrell, DJ, Verma, SP, Weaver, SD and Johnson, RW (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
Seltmann, R, Konopelko, D, Biske, G, Divaev, F and Sergeev, S (2011) Hercynian post-collisional magmatism in the context of Paleozoic magmatic evolution of the Tien Shan orogenic belt. Journal of Asian Earth Sciences, 42, 821–38.CrossRefGoogle Scholar
Sengör, AMC, Natal’in, BA and Burtman, VS (1993) Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature 364, 299–307.CrossRefGoogle Scholar
Shimoda, G, Tatsumi, Y, Nohda, S, Ishizaka, K and Jahn, BM (1998) Setouchi high-Mg andesites revisited: geochemical evidence for melting of subducting sediments. Earth and Planetary Science Letters 160, 479–92.CrossRefGoogle Scholar
Shiraki, K, Kuroda, N, Urano, H and Manuyama, S (1980) Clinoenstatite in boninites from the Bonin Islands, Japan. Nature 285, 31–32.CrossRefGoogle Scholar
Shirey, SB and Hanson, GN (1984) Mantle-derived Archaean monozodiorites and trachyandesites. Nature 310, 222–4.CrossRefGoogle Scholar
Solomovich, LI (2007) Postcollisional magmatism in the South Tien Shan Variscan Orogenic Belt, Kyrgyzstan: evidence for high-temperature and high-pressure collision. Journal of Asian Earth Sciences 30, 142–53.CrossRefGoogle Scholar
Solomovich, LI and Trifonov, BA (2002) Postcollisional granites in the South Tien Shan Variscan Collisional Belt, Kyrgyzstan. Journal of Asian Earth Sciences 21, 7–21.CrossRefGoogle Scholar
Song, DF, Xiao, WJ, Han, CM, Li, JL, Qu, JF, Guo, QQ, Lin, LN and Wang, ZM (2012) 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, Tian, ZH and Wang, ZM (2013) 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
Song, SG, Wang, MM, Xu, X, Wang, C, Niu, Y, Allen, MB and Su, L (2016) Ophiolites in the Xing’an-Inner Mongolia accretionary belt of the CAOB: implications for two cycles of seafloor spreading and accretionary orogenic events. Tectonics 34, 2221–48.CrossRefGoogle Scholar
Stern, RA and Hanson, GN (1991) Archean high-Mg granodiorite: a derivative of light rare earth element-enriched monzodiorite of mantle origin. Journal of Petrology 32, 201–38.CrossRefGoogle Scholar
Stern, RA, Hanson, GN and Shirey, SB (1989) Petrogenesis of mantle-derived, LILE-enriched Archean monzodiorites and trachyandesites (sanukitoids) in southwestern Superior Province. Canadian Journal of Earth Sciences 26, 1688–712.CrossRefGoogle Scholar
Su, BX, Qin, KZ, Sakyi, PA, Li, XH, Yang, YH, Sun, H, Tang, DM, Liu, PP, Xiao, QH and Malaviarachchi, SP (2011) U–Pb ages and Hf–O isotopes of zircons from Late Paleozoic mafic–ultramafic units in the southern Central Asian Orogenic Belt: tectonic implications and evidence for an Early Permian mantle plume. Gondwana Research 20, 516–31.CrossRefGoogle Scholar
Su, BX, Qin, KZ, Santosh, M, Sun, H and Tang, DM (2013) The Early Permian mafic-ultramafic complexes in the Beishan Terrane, NW China: Alaskan-type intrusives or rift cumulates? Journal of Asian Earth Sciences 66, 175–87.CrossRefGoogle Scholar
Su, W, Gao, J, Klemd, R, Li, JL, Zhang, X, Li, XH, Chen, NS and Zhang, L (2010) U–Pb zircon geochronology of Tianshan eclogites in NW China: implication for the collision between the Yili and Tarim blocks of the southwestern Altaids. European Journal of Mineralogy 22, 473–8.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 AD Saunders and MJ Norry), pp. 313–345. Geological Society of London, Special Publications no. 42.Google Scholar
Tanaka, T, Togashi, S, Kamioka, H, Amakawa, H, Kagami, H, Hamamoto, T, Yuhara, M, Orihashi, Y, Yoneda, S and Shimizu, H (2000) JNdi-1: a neodymium isotopic reference in consistency with LaJolla neodymium. Chemical Geology 168, 279–81.CrossRefGoogle Scholar
Tang, GJ and Wang, Q (2010) High-Mg andesites and their geodynamic implications. Acta Petrologica Sinica 26, 2495–512 (in Chinese with English abstract).Google Scholar
Tang, GJ, Wang, Q, Wyman, DA, Sun, M, Zhao, ZH and Jiang, ZQ (2013) Petrogenesis of gold-mineralized magmatic rocks of the Taerbieke area, northwestern Tianshan (western China): constraints from geochronology, geochemistry and Sr–Nd–Pb–Hf isotopic compositions. Journal of Asian Earth Sciences 74, 113–28.CrossRefGoogle Scholar
Tatsumi, Y (2001) Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction: generation of high-Mg andesites in the Setouchi volcanic belt, southwest Japan. Geology 29, 323–6.2.0.CO;2>CrossRefGoogle Scholar
Tatsumi, Y (2006) High-Mg andesites in the Setouchi volcanic belt, southwestern Japan: Analogy to Archean magmatism and continental crust formation? Annual Review of Earth & Planetary Science, 34, 467–99.CrossRefGoogle Scholar
Tatsumi, Y (2008) The formation of the continental crust: the connection with the sanukite. China Science Bulletin 53, 977–90 (in Chinese with English abstract).Google Scholar
Tatsumi, Y and Ishizaka, K (1981) Existence of andesitic primary magma: an example from southwest Japan. Earth and Planetary Science Letters 53, 124–30.CrossRefGoogle Scholar
Tatsumi, Y and Ishizaka, K (1982) Origin of high-magnesian andesites in the Setouchi volcanic belt, southwest Japan, I. Petrographical and chemical characteristics. Earth and Planetary Science Letters 60, 293–304.CrossRefGoogle Scholar
Tatsumi, Y, Shukuno, H, Sato, K, Shibata, T and Yoshikawa, M (2003) The petrology and geochemistry of high-magnesium andesites at the western tip of the Setouchi volcanic belt, SW Japan. Journal of Petrology 44, 1561–78.CrossRefGoogle 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.CrossRefGoogle Scholar
Wang, B and Ruffet, G (2010) Structural and geochronological study of high-pressure metamorphic rocks in the Kekesu Section (northwestern China): implications for the Late Paleozoic tectonics of the southern Tianshan. Journal of Geology 118, 59–77.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, 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 (in Chinese with English abstract).Google Scholar
Wang, KL, Sun, LC, O’Reilly, SY, Sun, SS, Ryuichi, S and Chen, CH (2004a) Geochemical constraints for the genesis of post-collisional magmatism and the geodynamic evolution of the northern Taiwan region. Journal of Petrology 45, 975–1011.CrossRefGoogle Scholar
Wang, LS, Yang, JG, Xie, CL, Lei, YX, Wang, YC, Cao, HX, Yang, PF, Qi, JL and Jin, SL (2009) Geochronology and geochemistry of Haergentoukoubu granites in the Beishan area, Gansu, China and their geological significance. Acta Geologica Sinica 83, 377–87 (in Chinese with English abstract).Google Scholar
Wang, Q, Wyman, DA, Xu, J, Dong, Y, Vasconcelos, PM, Pearson, N, Wan, Y, Dong, H, Li, C and Yu, Y (2008a) Eocene melting of subducting continental crust and early uplifting of central Tibet: evidence from central-western Qiangtang high-K calc-alkaline andesites, dacites and rhyolites. Earth and Planetary Science Letters 272, 158–71.CrossRefGoogle Scholar
Wang, Q, Wyman, DA, Xu, J, Wan, Y, Li, C, Feng, Z, Jiang, Z, Qiu, H, Chu, Z and Zhao, Z (2008b) Triassic Nb-enriched basalts, magnesian andesites, and adakites of the Qiangtang terrane (Central Tibet): evidence for metasomatism by slab-derived melts in the mantle wedge. Contributions to Mineralogy and Petrology 155, 473–90.CrossRefGoogle Scholar
Wang, Q, Wyman, DA, Zhao, ZH, Xu, JF, Bai, ZH., Xiong, XL, Dai, TM, Li, CF and Chu, ZY (2007) Petrogenesis of Carboniferous adakites and Nb-enriched arc basalts in the Alataw area, northern Tianshan Range (western China): implications for Phanerozoic crustal growth in the Central Asia orogenic belt. Chemical Geology 236, 42–64.CrossRefGoogle Scholar
Wang, Q, Zhao, ZH, Bai, ZH, Xiong, XL, Mei, HJ, Xu, JF, Bao, ZW and Wang, YX (2004b) Carboniferous adakite-high-Mg andesite-Nb-enriched basaltic rocks suites in the Alatao, Xinjiang: interaction between plate melt and mantle peridotite and crustal growth. China Science Bulletin 48, 1342–9 (in Chinese).Google Scholar
Wang, Q, Zhao, ZH, Xu, JF, Wyman, DA, Xiong, XL, Zi, F and Bai, ZH (2006) Carboniferous adakite-high-Mg andesite-Nb-enriched basaltic rock suites in theNorthern Tianshan area: Implications for Phanerozoic crustal growth in the Central Asia Orogenic Belt and Cu-Au mineralization. Acta Petrologica Sinica 22, 11–30 (in Chinese with English abstract).Google Scholar
Wang, SD, Zhang, KX, Song, BW, Li, SC, Li, M and Zhou, J (2018) 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
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 164, 31–47.CrossRefGoogle Scholar
Windley, BF, Allen, MB, Zhang, C, Zhao, ZY and Wang, GR (1990) Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan range, Central Asia. Geology 18, 128–31.2.3.CO;2>CrossRefGoogle Scholar
Xia, LQ, Xia, ZC, Xu, XY, Li, XM and Ma, ZP (2008) Relative contributions of crust and mantle to the generation of the Tianshan Carboniferous rift-related basic lavas, northwestern China. Journal of Asian Earth Sciences 31, 357–78.CrossRefGoogle Scholar
Xia, LQ, Xu, XY and Xia, ZC (2004) Petrogenesis of Carboniferous rift-related volcanic rocks in the Tianshan, northwestern China. Geological Society of America Bulletin, 116, 419–33.CrossRefGoogle Scholar
Xia, LQ, Xu, XY, Xia, ZC, Li, XM, Ma, ZP and Wang, LS (2003) Carboniferous post-collisional rift volcanism of the Tian Shan Mountains, northwestern China. Acta Geologica Sinica (English Edition) 77, 338–60.Google Scholar
Xiao, WJ, Han, CM, Chao, Y, Min, S, Lin, SF, Chen, HL, Li, ZL, Li, JL and Shu, S (2008) Middle Cambrian to Permian subduction-related accretionary orogenesis of North Xinjiang NW China: implications for the tectonic evolution of Central Asia. Journal of Asian Earth Sciences 32, 102–17.CrossRefGoogle Scholar
Xiao, WJ, Huang, BC, Han, CM, Sun, S and Li, JL (2010a) 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, N and Lin, SF (2010b) Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage. American Journal of Science 310, 1553–94.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Allen, M and Han, CM (2013) Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage. Gondwana Research 23, 1316–41.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Badarch, G, Sun, S, Li, JL, Qin, KZ and Wang, Z (2004) Paleozoic accretionary and convergent tectonics of the southern Altaids: implications for the growth of Central Asia. Journal of the Geological Society 161, 339–42.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Huang, B, Han, CM, Yuan, C, Chen, H, Sun, M, Sun, S and Li, JL (2009) End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia. International Journal of Earth Sciences 98, 1189–217.CrossRefGoogle Scholar
Xiao, XC, He, GQ, Xu, X, Zhu, BQ, Li, JY and Zhao, M (2010c) Crustal Structure and Geological Evolution in Xinjiang, China. Beijing, Geological Publishing House, pp. 104–124 (in Chinese with English abstract).Google Scholar
Xiao, XC, Tang, YQ, Feng, YM, Zhu, BQ, Li, JY and Zhao, M (1992) Tectonic Evolution of the Northern Xinjiang and its Adjacent Regions. Beijing: Geological Publishing House, 169 pp. (in Chinese with English abstract).Google Scholar
Xie, W, Song, XY, Deng, YF, Wang, YS, Ba, DH, Zheng, WQ and Li, XB (2012) Geochemistry and petrogenetic implications of a Late Devonian mafic–ultramafic intrusion at the southern margin of the Central Asian Orogenic Belt. Lithos 144–145, 209–30.CrossRefGoogle Scholar
Xu, JF, Shinjo, R, Defant, MJ, Wang, Q and Rapp, RP (2002) Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: partial melting of delaminated lower continental crust? Geology 30, 1111–4.2.0.CO;2>CrossRefGoogle Scholar
Xue, SC, Li, CS, Qin, KZ and Tang, DM (2016) A non-plume model for the Permian protracted (266–286 Ma) basaltic magmatism in the Beishan–Tianshan region, Xinjiang, Western China. Lithos 256, 243–49.CrossRefGoogle Scholar
Yang, HQ, Zhao, GB, Li, WM, Yang, JG, Li, Y, Wang, XH, Jiang, HB and Tan, WJ (2010) Formation age and source tracing of the tungsten-bearing granite belt in the Pantuoshan–Yingzuihongshan Area, Inner Mongolia. Geology and Exploration 46, 407–13 (in Chinese with English abstract).Google Scholar
Yang, L, Song, S, Su, L, Allen, MB, Niu, Y, Zhang, G and Zhang, Y (2019) Heterogeneous oceanic arc volcanic rocks in the South Qilian Accretionary Belt (Qilian Orogen, NW China). Journal of Petrology 60, 85–116.CrossRefGoogle Scholar
Yogodzinski, GM, Kay, RW, Volynets, ON, Koloskov, AV and Kay, SM (1995) Magnesian andesite in the western Aleutian Komandorsky region: implications for slab melting and processes in the mantle wedge. Geological Society of America Bulletin 107, 505–19.2.3.CO;2>CrossRefGoogle Scholar
Yogodzinski, GM and Kelemen, PB (1998) Slab melting in the Aleutians: implications of an ion probe study of clinopyroxene in primitive adakite and basalt. Earth and Planetary Science Letters 158, 53–65.CrossRefGoogle Scholar
Yu, JY, Guo, L, Li, JX, Li, YG, Smithies, RH, Wingate, MTD, Meng, Y and Chen, SF (2016) The petrogenesis of sodic granites in the Niujuanzi area and constraints on the Paleozoic tectonic evolution of the Beishan region, NW China. Lithos 256–257, 250–68.CrossRefGoogle Scholar
Yu, JY, Ji, B and Guo, L (2017) The petrogenesis and tectonic significances of Silurian west-Luotuojuan rocks from Beishan Niujuanzi area in Gansu province, NW China. Journal of Geomechanics 23, 253–63 (in Chinese with English abstract).Google Scholar
Yu, JY, Li, XM, Wang, GQ, Wu, P and Yan, QJ (2012) Zircon U-Pb ages of Huitongshan and Zhangfangshan ophiolite in Beishan of Gansu–Inner Mongolia border area and their significance. Geological Bulletin of China 31, 2038–45 (in Chinese with English abstract).Google Scholar
Yuan, Y, Zong, KQ, He, ZY, Klemd, R, Jiang, HY, Zhang, W, Liu, YS, Hu, ZC and Zhang, ZM (2018) Geochemical evidence for Paleozoic crustal growth and tectonic conversion in the Northern Beishan Orogenic Belt, southern Central Asian Orogenic Belt. Lithos 302–303, 189–202.CrossRefGoogle Scholar
Zhang, LF, Ai, YL, Li, XP, Rubatto, D, Song, B, Williams, S, Song, S, Ellis, D and Liou, J (2007) Triassic collision of western Tianshan orogenic belt, China: evidence from SHRIMP U–Pb dating of zircon from HP/UHP eclogitic rocks. Lithos 96, 266–80.CrossRefGoogle Scholar
Zhang, Y, Yuan, C, Sun, M, Long, X, Wang, Y, Jiang, Y and Lin, Z (2017) Arc magmatism associated with steep subduction: insights from trace element and Sr-Nd-Hf-B isotope systematics. Journal of Geophysical Research Solid Earth 122, 1816–34.Google Scholar
Zhao, CH and Chen, TF (1992) A discussion on magma-tectonic type of Cenozoic volcanism from Tengchong area (Yunnan province): A new type of post-collision arc-volcanism. Geoscience 6, 119–29 (in Chinese with English abstract).Google Scholar
Zhao, ZH, Guo, ZJ and Wang, Y (2007) Geochronology, geochemical characteristics and tectonic implications of the granitoids from Liuyuan area, Beishan, Gansu province, northwest China. Acta Petrologica Sinica 23, 1847–60 (in Chinese with English abstract).Google Scholar
Zhou, DW, Liu, YQ, Xing, XJ, Hao, JR, Dong, YP and Ouyang, ZJ (2006) Formation of the Permian basalts and implications of geochemical tracing for paleo-tectonic setting and regional tectonic background in the Turpan-Hami and Santanghu basins, Xinjiang. Science in China Series D 49, 584–96.CrossRefGoogle Scholar
Zhou, W, Zhao, X, Fu, D, Sun, J, Li, Z, Huang, B, Mengchun, G and Santosh, M (2018) Geochronology and geochemistry of the Carboniferous Ulann Tolgoi granite complex from northern Inner Mongolia, China: petrogenesis and tectonic implications for the Uliastai continental margin. Geological Journal 53, 2690–709.CrossRefGoogle Scholar
Zindler, A and Hart, S (1986) Chemical geodynamics. Annual Review of Earth and Planetary Sciences 14, 493–571.CrossRefGoogle Scholar
Zuo, GC, He, GQ and Li, HC (1990a) Plate Tectonics and Metallogenesis Regularities in Beishan Region. Beijing: Peking University Press, pp. 189–194 (in Chinese with English abstract).Google Scholar
Zuo, GC and Li, MS (1996) Formation and Environment of the Early Paleozoic Lithosphere in the Beishan Area, Gansu-Inner Mongolia, China. Lanzhou: Gansu Science and Technology Press, pp. 23–67 (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
Zuo, GC, Zhang, SL, He, GQ and Zhang, Y (1990b) Early Paleozoic plate tectonics in Beishan area. Scientia Geologica Sinica 25, 305–14 (in Chinese with English abstract).Google Scholar