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Volume 37 Issue 3
Jun 2026
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Article Contents
Zhicheng Yu, Jingen Dai, Jie Shen, Kai Yang, Xu Han, Shiying Xu. Subduction-Accretion Process of the Neo-Tethyan Ocean: Insights from the Purang Mélange in the Western Yarlung Zangbo Suture Zone. Journal of Earth Science, 2026, 37(3): 1179-1192. doi: 10.1007/s12583-025-0253-y
Citation: Zhicheng Yu, Jingen Dai, Jie Shen, Kai Yang, Xu Han, Shiying Xu. Subduction-Accretion Process of the Neo-Tethyan Ocean: Insights from the Purang Mélange in the Western Yarlung Zangbo Suture Zone. Journal of Earth Science, 2026, 37(3): 1179-1192. doi: 10.1007/s12583-025-0253-y

Subduction-Accretion Process of the Neo-Tethyan Ocean: Insights from the Purang Mélange in the Western Yarlung Zangbo Suture Zone

doi: 10.1007/s12583-025-0253-y
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  • Corresponding author: Jingen Dai, djgtibet@163.com
  • Received Date: 20 Jun 2024
  • Accepted Date: 25 Mar 2025
  • Issue Publish Date: 30 Jun 2026
  • The Purang mélange, located within the western Yarlung Zangbo suture zone (YZSZ) in southern Tibet, provides valuable insights into the subduction-accretion process along the active southern margin of Asia during the Cretaceous–Paleocene Neo-Tethyan subduction. This mélange consists of sandstone, chert, basalt, and limestone blocks embedded in a mud matrix. We performed petrological and detrital zircon U-Pb geochronological analyses for the sandstone blocks to trace their provenances, while the whole-rock geochemical analyses for the chert and basalt to determine their sedimentary and tectonic settings. The sandstone blocks are primarily composed of quartz, with a few lithic fragments. Both of the sandstone samples exhibit detrital zircon U-Pb age ranges consistent with those of the Tethyan Himalaya. These results suggest that the sandstone blocks of the Purang mélange were derived from the passive continental margin of India. The basalt blocks exhibit three styles according to their geochemical characteristics, indicating that they originated from a subducted Neo-Tethyan slab. The chert blocks, however, display geochemical affinities of both pelagic and continental margins, indicative of a dual origin from both the subducted and overlying slabs. Based on the above observations, we propose a two-stage subduction-accretion process of the Neo-Tethyan Ocean. The basalt blocks were scraped from the subducted oceanic slab and incorporated into the subduction complexes during the Neo-Tethyan subduction stage of the Cretaceous, whereas the sandstone blocks of the passive continental margin reached the trench and were subsequently incorporated into the Purang mélange during the India-Asia collision stage of the Paleogene.

     

  • Electronic Supplementary Materials: Supplementary materials (Tables S1–S3) are available in the online version of this article at https://doi.org/10.1007/s12583-025-0253-y.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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  • Aikman, A. B., Harrison, T. M., Lin, D., 2008. Evidence for Early (> 44 Ma) Himalayan Crustal Thickening, Tethyan Himalaya, Southeastern Tibet. Earth and Planetary Science Letters, 274(1/2): 14–23. https://doi.org/10.1016/j.epsl.2008.06.038
    Aitchison, J. C., Badengzhu, Davis, A. M., et al., 2000. Remnants of a Cretaceous Intra-Oceanic Subduction System within the Yarlung-Zangbo Suture (Southern Tibet). Earth and Planetary Science Letters, 183(1/2): 231–244.https://doi.org/10.1016/s0 012-821x(00)00287-9 doi: 10.1016/s0012-821x(00)00287-9
    Aitchison, J. C., McDermid, I. R. C., Ali, J. R., et al., 2007. Shoshonites in Southern Tibet Record Late Jurassic Rifting of a Tethyan Intraoceanic Island Arc. The Journal of Geology, 115(2): 197–213. https://doi.org/10.1086/510642
    An, W., Hu, X. M., Garzanti, E., 2017. Sandstone Provenance and Tectonic Evolution of the Xiukang Mélange from Neotethyan Subduction to India-Asia Collision (Yarlung-Zangbo Suture, South Tibet). Gondwana Research, 41: 222–234. https://doi.org/10.1016/j.gr.2015.08.010
    Armstrong, H. A., Owen, A. W., Floyd, J. D., 1999. Rare Earth Geochemistry of Arenig Cherts from the Ballantrae Ophiolite and Leadhills Imbricate Zone, Southern Scotland: Implications for Origin and Significance to the Caledonian Orogeny. Journal of the Geological Society, 156(3): 549–560.https://doi.org/10.1 144/gsjgs.156.3.0549 doi: 10.1144/gsjgs.156.3.0549
    Bédard, Hébert, R., Guilmette, C., et al., 2009. Petrology and Geochemistry of the Saga and Sangsang Ophiolitic Massifs, Yarlung Zangbo Suture Zone, Southern Tibet: Evidence for an Arc-Back-Arc Origin. Lithos, 113(1/2): 48–67.https://doi.org/10. 1016/j.lithos.2009.01.011 doi: 10.1016/j.lithos.2009.01.011
    Cai, F. L., Ding, L., Leary, R. J., et al., 2012. Tectonostratigraphy and Provenance of an Accretionary Complex within the Yarlung-Zangpo Suture Zone, Southern Tibet: Insights into Subduction-Accretion Processes in the Neo-Tethys. Tectonophysics, 574/575: 181–192. https://doi.org/10.1016/j.tecto.2012.08.016
    Cai, F. L., Ding, L., Yue, Y. H., 2011. Provenance Analysis of Upper Cretaceous Strata in the Tethys Himalaya, Southern Tibet: Implications for Timing of India-Asia Collision. Earth and Planetary Science Letters, 305(1/2): 195–206. https://doi.org/10.1016/j.epsl.2011.02.055
    Chan, G. H. N., Aitchison, J. C., Crowley, Q. G., et al., 2015. U-Pb Zircon Ages for Yarlung Tsangpo Suture Zone Ophiolites, Southwestern Tibet and Their Tectonic Implications. Gondwana Research, 27(2): 719–732.https://doi.org/10.1016/j.gr.2013.0 6.016 doi: 10.1016/j.gr.2013.06.016
    Chen, X., Wang, C. S., Hu, X. M., et al., 2007. Cretaceous Oceanic Red Beds: Distribution, Lithostratigraphy and Paleoenvironments. Acta Geologica Sinica (English Edition), 81(6): 1070–1086. https://doi.org/10.1111/j.1755-6724.2007.tb01029.x
    Chung, S. L., Chu, M. F., Zhang, Y. Q., et al., 2005. Tibetan Tectonic Evolution Inferred from Spatial and Temporal Variations in Post-Collisional Magmatism. Earth-Science Reviews, 68(3/4): 173–196. https://doi.org/10.1016/j.earscirev.2004.05.001
    Cui, X. H., Luo, H., Aitchison, J. C., et al., 2021a. Middle Jurassic Radiolarians and Chert Geochemistry, Dajiweng Ophiolite, SW Tibet: Implications for Neotethyan Ocean Evolution. Journal of Asian Earth Sciences, 221: 104947.https://doi.org/10.1016/j.jse aes.2021.104947 doi: 10.1016/j.jseaes.2021.104947
    Cui, X. H., Luo, H., Aitchison, J. C., et al., 2021b. Early Cretaceous Radiolarians and Chert Geochemistry from Western Yarlung Tsangpo Suture Zone in Jiangyema Section, Purang County, SW Tibet. Cretaceous Research, 125: 104840. https://doi.org/10.1016/j.cretres.2021.104840
    Cui, X., 2021. Radiolarians and Geochemical Characteristics of the Cherts from the Western Yarlung Tsangpo Suture Zone, Tibet. University of Chinese Academy of Sciences, Nanjing (in Chinese with English Abstract)
    Dai, J. G., Wang, C. S., Li, Y. L., 2012. Relicts of the Early Cretaceous Seamounts in the Central-Western Yarlung Zangbo Suture Zone, Southern Tibet. Journal of Asian Earth Sciences, 53: 25–37. https://doi.org/10.1016/j.jseaes.2011.12.024
    Dai, J. G., Wang, C. S., Polat, A., et al., 2013. Rapid Forearc Spreading between 130 and 120Ma: Evidence from Geochronology and Geochemistry of the Xigaze Ophiolite, Southern Tibet. Lithos, 172/173: 1–16. https://doi.org/10.1016/j.lithos.2013.03.011
    DeCelles, P. G., Gehrels, G. E., Quade, J., et al., 2000. Tectonic Implications of U-Pb Zircon Ages of the Himalayan Orogenic Belt in Nepal. Science, 288(5465): 497–499. https://doi.org/10.1126/science.288.5465.497
    DeCelles, P. G., Kapp, P., Gehrels, G. E., et al., 2014. Paleocene-Eocene Foreland Basin Evolution in the Himalaya of Southern Tibet and Nepal: Implications for the Age of Initial India-Asia Collision. Tectonics, 33(5): 824–849.https://doi.org/10.1002/201 4tc003522 doi: 10.1002/2014tc003522
    Dickinson, W. R., 1985. Interpreting Provenance Relations from Detrital Modes of Sandstones. Provenance of Arenites. Dordrecht: Springer Netherlands: 333–361.https://doi.org/10.1007/978-94-017-2809-6_15
    Dilek, Y., Festa, A., Ogawa, Y., et al., 2012. Chaos and Geodynamics: Mélanges, Mélange-Forming Processes and Their Significance in the Geological Record. Tectonophysics, 568/569: 1–6. https://doi.org/10.1016/j.tecto.2012.08.002
    Dilek, Y., Thy, P., 2009. Island Arc Tholeiite to Boninitic Melt Evolution of the Cretaceous Kizildag (Turkey) Ophiolite: Model for Multi-Stage Early Arc-Forearc Magmatism in Tethyan Subduction Factories. Lithos, 113(1/2): 68–87. https://doi.org/10.1016/j.lithos.2009.05.044
    Du, X. J., Chen, X., Wang, C. S., et al., 2015. Geochemistry and Detrital Zircon U-Pb Dating of Lower Cretaceous Volcaniclastics in the Babazhadong Section, Northern Tethyan Himalaya: Implications for the Breakup of Eastern Gondwana. Cretaceous Research, 52: 127–137.https://doi.org/10.1016/j.cretres.2014.0 8.002 doi: 10.1016/j.cretres.2014.08.002
    Dubois-Côté, V., Hébert, R., Dupuis, C., et al., 2005. Petrological and Geochemical Evidence for the Origin of the Yarlung Zangbo Ophiolites, Southern Tibet. Chemical Geology, 214(3/4): 265–286. https://doi.org/10.1016/j.chemgeo.2004.10.004
    Dupuis, C., Hébert, R., Dubois-Côté, V., et al., 2006. Geochemistry of Sedimentary Rocks from Mélange and Flysch Units South of the Yarlung Zangbo Suture Zone, Southern Tibet. Journal of Asian Earth Sciences, 26(5): 489–508. https://doi.org/10.1016/j.jseaes.2004.11.002
    Gao, R., Lu, Z., Klemperer, S. L., et al., 2016. Crustal-Scale Duplexing beneath the Yarlung Zangbo Suture in the Western Himalaya. Nature Geoscience, 9(7): 555–560. https://doi.org/10.1038/ngeo2730
    Garzanti, E., 1999. Stratigraphy and Sedimentary History of the Nepal Tethys Himalaya Passive Margin. Journal of Asian Earth Sciences, 17(5/6): 805–827. https://doi.org/10.1016/s1367-9120(99)00017-6
    Garzanti, E., 2019. Petrographic Classification of Sand and Sandstone. Earth-Science Reviews, 192: 545–563. https://doi.org/10.1016/j.earscirev.2018.12.014
    Gehrels, G., Kapp, P., DeCelles, P., et al., 2011. Detrital Zircon Geochronology of Pre-Tertiary Strata in the Tibetan-Himalayan Orogen. Tectonics, 30(5): TC5016.https://doi.org/10.102 9/2011tc002868 doi: 10.1029/2011tc002868
    Guo, X. D., Ding, L., Laskowski, A. K., et al., 2022. Provenance of Late Cretaceous Accretionary Complex within the Yarlung-Zangpo Suture Zone, Bainang, Southern Tibet: Implications for the Subduction-Accretion of the Neo-Tethyan Ocean. Gondwana Research, 106: 78–91.https://doi.org/10.1016/j.gr.20 22.01.004 doi: 10.1016/j.gr.2022.01.004
    Guo, X., Ding, L., Cai, F., et al., 2019. Subduction and Accretion Process of the Western Segment of the Yarlung Zangbo Suture Zone in Zhongba Area, Tibet. Chinese Journal of Geology, 54(4): 1031–1047 (in Chinese with English Abstract)
    Hébert, R., Bezard, R., Guilmette, C., et al., 2012. The Indus-Yarlung Zangbo Ophiolites from Nanga Parbat to Namche Barwa Syntaxes, Southern Tibet: First Synthesis of Petrology, Geochemistry, and Geochronology with Incidences on Geodynamic Reconstructions of Neo-Tethys. Gondwana Research, 22(2): 377–397.https://doi.org/10.1016/j.gr.2011.1 0.013 doi: 10.1016/j.gr.2011.10.013
    Hou, Y., 2015. Tectonic Property Research on Zhongba Microterrane, Southern Tibet: Evidences from Detrital Zircon U-Pb Geochronology. China University of Geosciences (Beijing), Beijing (in Chinese with English Abstract)
    Hu, X. M., Jansa, L., Wang, C. S., 2008. Upper Jurassic–Lower Cretaceous Stratigraphy in South-Eastern Tibet: A Comparison with the Western Himalayas. Cretaceous Research, 29(2): 301–315. https://doi.org/10.1016/j.cretres.2007.05.005
    Hu, X. M., Jansa, L., Chen, L., et al., 2010. Provenance of Lower Cretaceous Wölong Volcaniclastics in the Tibetan Tethyan Himalaya: Implications for the Final Breakup of Eastern Gondwana. Sedimentary Geology, 223(3/4): 193–205. https://doi.org/10.1016/j.sedgeo.2009.11.008
    Ingersoll, R. V., Bullard, T. F., Ford, R. L., et al., 1984. The Effect of Grain Size on Detrital Modes: A Test of the Gazzi-Dickinson Point-Counting Method. SEPM Journal of Sedimentary Research, 54(1): 103–116.https://doi.org/10.1306/212f83b9-2b2 4-11d7-8648000102c1865d doi: 10.1306/212f83b9-2b24-11d7-8648000102c1865d
    Kretz, R., 1983. Symbols for Rock-Forming Minerals. American Mineralogist, 68(1–2): 277–279
    Kusky, T., Wang, J. P., Wang, L., et al., 2020. Mélanges through Time: Life Cycle of the World’s Largest Archean Mélange Compared with Mesozoic and Paleozoic Subduction-Accretion-Collision Mélanges. Earth-Science Reviews, 209: 103303. https://doi.org/10.1016/j.earscirev.2020.103303
    Laskowski, A. K., Orme, D. A., Cai, F. L., et al., 2019. The Ancestral Lhasa River: A Late Cretaceous Trans-Arc River that Drained the Proto-Tibetan Plateau. Geology, 47(11): 1029–1033. https://doi.org/10.1130/g46823.1
    Leier, A. L., Kapp, P., Gehrels, G. E., et al., 2007. Detrital Zircon Geochronology of Carboniferous–Cretaceous Strata in the Lhasa Terrane, Southern Tibet. Basin Research, 19(3): 361–378. https://doi.org/10.1111/j.1365-2117.2007.00330.x
    Li, G. W., Sandiford, M., Boger, S., et al., 2015. Provenance of the Upper Cretaceous to Lower Tertiary Sedimentary Relicts in the Renbu Mélange Zone, within the Indus-Yarlung Suture Zone. The Journal of Geology, 123(1): 39–54. https://doi.org/10.1086/680207
    Li, X., Wang, C., Li, Y., et al., 2014. Definition and Composition of the Zhongba Microterrane in the Southwest Tibet. Acta Geological Sinica, 88(8): 1372–1381 (in Chinese with English Abstract)
    Lin, C., Zhang, J., Huang, T., et al., 2020. Tectonic Affinity of Zhongba Microterrane: Constraint from Detritai Zircon Geochronoiogy of the SiIurian–Carboniferous Strata in the Mayum Region, Southern Tibet. Chinese Journal of Geology, 55(2): 574–597 (in Chinese with English Abstract)
    Liu, C. Z., Wu, F. Y., Wilde, S. A., et al., 2010. Anorthitic Plagioclase and Pargasitic Amphibole in Mantle Peridotites from the Yungbwa Ophiolite (Southwestern Tibetan Plateau) Formed by Hydrous Melt Metasomatism. Lithos, 114(3/4): 413–422. https://doi.org/10.1016/j.lithos.2009.10.008
    Liu, F., Dilek, Y., Yang, J. S., et al., 2021. A Middle Triassic Seamount within the Western Yarlung Zangbo Suture Zone, Tibet: The Earliest Seafloor Spreading Record of Neotethys to the North of East Gondwana. Lithos, 388/389: 106062.https://doi.org/10.101 6/j.lithos.2021.106062 doi: 10.1016/j.lithos.2021.106062
    Liu, F., Yang, J. S., Dilek, Y., et al., 2015. Geochronology and Geochemistry of Basaltic Lavas in the Dongbo and Purang Ophiolites of the Yarlung-Zangbo Suture Zone: Plume-Influenced Continental Margin-Type Oceanic Lithosphere in Southern Tibet. Gondwana Research, 27(2): 701–718. https://doi.org/10.1016/j.gr.2014.08.002
    Liu, G. H., Einsele, G., 1994. Sedimentary History of the Tethyan Basin in the Tibetan Himalayas. Geologische Rundschau, 83(1): 32–61. https://doi.org/10.1007/bf00211893
    Ma, X. D., Tan, X. D., Li, Y. L., et al., 2024. Paleolatitude of Mafic Dykes in the Xiugugabu Ophiolite: Implications for the Intraoceanic Trans-Tethyan Subduction Zone and Multistage India-Eurasia Collision. Tectonophysics, 889: 230466. https://doi.org/10.1016/j.tecto.2024.230466
    Malpas, J., Zhou, M. F., Robinson, P. T., et al., 2003. Geochemical and Geochronological Constraints on the Origin and Emplacement of the Yarlung Zangbo Ophiolites, Southern Tibet. Geological Society, London, Special Publications, 218(1): 191–206. https://doi.org/10.1144/gsl.sp.2003.218.01.11
    Meng, Z. Y., Wang, J. G., Garzanti, E., et al., 2021. Late Triassic Rifting and Volcanism on the Northeastern Indian Margin: A New Phase of Neo-Tethyan Seafloor Spreading and Its Paleogeographic Implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 570: 110367. https://doi.org/10.1016/j.palaeo.2021.110367
    Meng, Z. Y., Wang, J. G., Ji, W. Q., et al., 2019. The Langjiexue Group Is an in-situ Sedimentary Sequence rather than an Exotic Block: Constraints from Coeval Upper Triassic Strata of the Tethys Himalaya (Qulonggongba Formation). Science China Earth Sciences, 62(5): 783–797. https://doi.org/10.1007/s11430-018-9314-9
    Metcalf, K., Kapp, P., 2017. The Yarlung Suture Mélange, Lopu Range, Southern Tibet: Provenance of Sandstone Blocks and Transition from Oceanic Subduction to Continental Collision. Gondwana Research, 48: 15–33.https://doi.org/10.1016/j.gr.201 7.03.002 doi: 10.1016/j.gr.2017.03.002
    Miller, C., 2003. Geochemistry and Tectonomagmatic Affinity of the Yungbwa Ophiolite, SW Tibet. Lithos, 66(3/4): 155–172. https://doi.org/10.1016/s0024-4937(02)00217-7
    Murphy, M. A., Yin, A., 2003. Structural Evolution and Sequence of Thrusting in the Tethyan Fold-Thrust Belt and Indus-Yalu Suture Zone, Southwest Tibet. Geological Society of America Bulletin, 115(1): 21–34.https://doi.org/10.1130/0016-7606(2003)1150021:seasot>2.0.co;2 doi: 10.1130/0016-7606(2003)1150021:seasot>2.0.co;2
    Murray, R. W., 1994. Chemical Criteria to Identify the Depositional Environment of Chert: General Principles and Applications. Sedimentary Geology, 90(3/4): 213–232. https://doi.org/10.1016/0037-0738(94)90039-6
    Murray, R. W., Buchholtz Ten Brink, M. R., Gerlach, D. C., et al., 1992. Rare Earth, Major, and Trace Element Composition of Monterey and DSDP Chert and Associated Host Sediment: Assessing the Influence of Chemical Fractionation during Diagenesis. Geochimica et Cosmochimica Acta, 56(7): 2657–2671. https://doi.org/10.1016/0016-7037(92)90351-I
    Myrow, P. M., Hughes, N. C., Searle, M. P., et al., 2009. Stratigraphic Correlation of Cambrian–Ordovician Deposits along the Himalaya: Implications for the Age and Nature of Rocks in the Mount Everest Region. Geological Society of America Bulletin, 121(3/4): 323–332. https://doi.org/10.1130/b26384.1
    Orme, D. A., Carrapa, B., Kapp, P., 2015. Sedimentology, Provenance and Geochronology of the Upper Cretaceous–Lower Eocene Western Xigaze Forearc Basin, Southern Tibet. Basin Research, 27(4): 387–411.https://doi.org/10.1111/bre.1 2080 doi: 10.1111/bre.12080
    Orme, D. A., Laskowski, A. K., Zilinsky, M. F., et al., 2021. Sedimentology and Provenance of Newly Identified Upper Cretaceous Trench Basin Strata, Dênggar, Southern Tibet: Implications for Development of the Eurasian Margin Prior to India-Asia Collision. Basin Research, 33(2): 1454–1473. https://doi.org/10.1111/bre.12521
    Pullen, A., Kapp, P., Gehrels, G. E., et al., 2008. Gangdese Retroarc Thrust Belt and Foreland Basin Deposits in the Damxung Area, Southern Tibet. Journal of Asian Earth Sciences, 33(5/6): 323–336. https://doi.org/10.1016/j.jseaes.2008.01.005
    Sharman, G. R., Sharman, J. P., Sylvester, Z., 2018. DetritalPy: A Python-Based Toolset for Visualizing and Analysing Detrital Geo-Thermochronologic Data. The Depositional Record, 4(2): 202–215. https://doi.org/10.1002/dep2.45
    Sun, G., Hu, X., 2012. Tectonic Aftnity of Zhongba Terrane: Evidences from the Detrital Zircon Geochronology and Hf Isotopes. Acta Petrological Sinica, 28(5): 1635–1646 (in Chinese with English Abstract)
    Sun, S. S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42(1): 313–345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
    Tapponnier, P., Mercier, J. L., Proust, F., et al., 1981. The Tibetan Side of the India-Eurasia Collision. Nature, 294(5840): 405–410. https://doi.org/10.1038/294405a0
    Vermeesch, P., 2013. Multi-Sample Comparison of Detrital Age Distributions. Chemical Geology, 341: 140–146. https://doi.org/10.1016/j.chemgeo.2013.01.010
    Wang, H. Q., Ding, L., Kapp, P., et al., 2018. Earliest Cretaceous Accretion of Neo-Tethys Oceanic Subduction along the Yarlung Zangbo Suture Zone, Sangsang Area, Southern Tibet. Tectonophysics, 744: 373–389.https://doi.org/10.1016/j.tecto.20 18.07.024 doi: 10.1016/j.tecto.2018.07.024
    Wang, Q., Zhu, D. C., Cawood, P. A., et al., 2021. Resolving the Paleogeographic Puzzle of the Lhasa Terrane in Southern Tibet. Geophysical Research Letters, 48(15): e2021GL094236. https://doi.org/10.1029/2021gl094236
    Webb, A. A. G., Yin, A., Dubey, C. S., 2013. U-Pb Zircon Geochronology of Major Lithologic Units in the Eastern Himalaya: Implications for the Origin and Assembly of Himalayan Rocks. Geological Society of America Bulletin, 125(3/4): 499–522. https://doi.org/10.1130/b30626.1
    Wu, F. -Y., Ji, W. -Q., Wang, J. -G., et al., 2014. Zircon U-Pb and Hf Isotopic Constraints on the Onset Time of India-Asia Collision. American Journal of Science, 314(2): 548–579. https://doi.org/10.2475/02.2014.04
    Xiao, S. Q., Li, Y. L., He, J., et al., 2023. Late Permian Rift-Related Volcanic Rocks from the Zhongba Terrane, Southern Tibet: Implications for the Opening of the Neotethys. International Geology Review, 65(10): 1682–1695.https://doi.org/10.1080/00 206814.2022.2103847 doi: 10.1080/00206814.2022.2103847
    Xiong, Z. Y., Liu, X. H., Ding, L., et al., 2022. The Rise and Demise of the Paleogene Central Tibetan Valley. Science Advances, 8(6): eabj0944. https://doi.org/10.1126/sciadv.abj0944
    Xu, Z. Q., Dilek, Y., Yang, J. S., et al., 2015. Crustal Structure of the Indus-Tsangpo Suture Zone and Its Ophiolites in Southern Tibet. Gondwana Research, 27(2): 507–524. https://doi.org/10.1016/j.gr.2014.08.001
    Yin, A., Harrison, T. M., 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annual Review of Earth and Planetary Sciences, 28: 211–280.https://doi.org/10.1146/annurev.earth.2 8.1.211 doi: 10.1146/annurev.earth.28.1.211
    Yu, Y., Xu, X., and Gao, R., 2020. Seismic Evidence for Tectonic Affinity of the Yungbwa Ophiolitic Complex. Chinese J. Geophys, 63(3): 840–846 (in Chinese with English Abstract)
    Zhang, L., Wang, G. H., Park, C., et al., 2020. Tectonic Evolution of North-Eastern Tethyan Himalaya: Evidence from U-Pb Geochronology and Hf Isotopic Geochemistry of Detrital Zircons. Geological Journal, 55(5): 3694–3715. https://doi.org/10.1002/gj.3617
    Zhu, D. C., Mo, X. X., Niu, Y. L., et al., 2009. Zircon U-Pb Dating and in-situ Hf Isotopic Analysis of Permian Peraluminous Granite in the Lhasa Terrane, Southern Tibet: Implications for Permian Collisional Orogeny and Paleogeography. Tectonophysics, 469(1/2/3/4): 48–60. https://doi.org/10.1016/j.tecto.2009.01.017
    Zhu, D. C., Zhao, Z. D., Niu, Y., et al., 2011a. Lhasa Terrane in Southern Tibet Came from Australia. Geology, 39(8): 727–730. https://doi.org/10.1130/g31895.1
    Zhu, D. C., Zhao, Z. D., Niu, Y. L., et al., 2011b. The Lhasa Terrane: Record of a Microcontinent and Its Histories of Drift and Growth. Earth and Planetary Science Letters, 301(1/2): 241–255. https://doi.org/10.1016/j.epsl.2010.11.005
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