Abstract
Numerous continents have rifted and drifted away from Gondwana to repeatedly open ocean basins over the past ∼500 million years. These Gondwana-derived continents drifted towards and collided with components of the Eurasian continent to successively close the preexisting oceans between the two. Plate tectonics satisfactorily describes the continental drift from Gondwana to Eurasia but does not define the geodynamic mechanism of continuously rifting to collisions of continents in the Tethyan Realm. After reappraisal of geological records of the rift, collision and subduction initiation from the surface and various geophysical observations from depth, we propose that Eurasia-directed subducting oceanic slabs would have driven Tethyan system in the Phanerozoic. The Eurasia-directed subduction would have dragged the passive Gondwana margin to rift and drift northwards, giving birth to new oceans since the Paleozoic. The closure of preexisting oceans between the Gondwana-derived continents and Eurasia led to continental collisions, which would have induced the initiation of oceanic subduction in the Tethyan Realm. Multiple episodic switches between collision-subduction-rift repeatedly led to the separation of continental fragments from Gondwana and dragged them to drift towards Eurasia. The final disappearance of Neo-Tethys would have induced collision of the Gondwana-derived continents with the Eurasian continent, giving rise to the Cenozoic Alpine-Zagros-Himalayan collisional system. Therefore, the Eurasia-directed oceanic subduction would have acted as a ‘one-way train’ that successively transferred the ruptured Gondwana continental fragments in the south, into the terminal in the north. In this regard, the engine of this “Tethyan one-way train” is the negative buoyancy of subducting oceanic slabs.
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References
Advokaat E L, Bongers M L M, Rudyawan A, BouDagher-Fadel M K, Langereis C G, van Hinsbergen D J J. 2018. Early Cretaceous origin of the Woyla Arc (Sumatra, Indonesia) on the Australian plate. Earth Planet Sci Lett, 498: 348–361
Barley M E, Pickard A L, Zaw K, Rak P, Doyle M G. 2003. Jurassic to Miocene magmatism and metamorphism in the Mogok metamorphic belt and the India-Eurasia collision in Myanmar. Tectonics, 22: 1019
Becker T W, Faccenna C. 2011. Mantle conveyor beneath the Tethyan collisional belt. Earth Planet Sci Lett, 310: 453–461
Brown D, Ryan P D. 2011. Arc-Continent Collision. Heidelberg: Springer. 493
Buiter S J H, Torsvik T H. 2014. A review of Wilson Cycle plate margins: A role for mantle plumes in continental break-up along sutures? Gondwana Res, 26: 627–653
Burg J P. 2018. Geology of the onshore Makran accretionary wedge: Synthesis and tectonic interpretation. Earth-Sci Rev, 185: 1210–1231
Capitanio F A, Morra G, Goes S, Weinberg R F, Moresi L. 2010. India-Asia convergence driven by the subduction of the Greater Indian continent. Nat Geosci, 3: 136–139
Chen Y W, Wu J, Suppe J. 2019. Southward propagation of Nazca subduction along the Andes. Nature, 565: 441–447
Chiu H Y, Chung S L, Zarrinkoub M H, Mohammadi S S, Khatib M M, Iizuka Y. 2013. Zircon U-Pb age constraints from Iran on the magmatic evolution related to Neotethyan subduction and Zagros orogeny. Lithos, 162-163: 70–87
Conrad C P, Lithgow-Bertelloni C. 2002. How mantle slabs drive plate tectonics. Science, 298: 207–209
Copley A, Avouac J P, Royer J Y. 2010. India-Asia collision and the Cenozoic slowdown of the Indian plate: Implications for the forces driving plate motions. J Geophys Res, 115: B03410
Courtillot V, Jaupart C, Manighetti I, Tapponnier P, Besse J. 1999. On causal links between flood basalts and continental breakup. Earth Planet Sci Lett, 166: 177–195
Dewey J F, Burke K. 1974. Hot spots and continental break-up: Implications for collisional orogeny. Geology, 2: 57–60
Dong Y, He D, Sun S, Liu X, Zhou X, Zhang F, Yang Z, Cheng B, Zhao G, Li J. 2018. Subduction and accretionary tectonics of the East Kunlun orogen, western segment of the Central China Orogenic System. Earth-Sci Rev, 186: 231–261
Faccenna C, Becker T W, Auer L, Billi A, Boschi L, Brun J P, Capitanio F A, Funiciello F, Horvàth F, Jolivet L, Piromallo C, Royden L, Rossetti F, Serpelloni E. 2014. Mantle dynamics in the Mediterranean. Rev Geophys, 52: 283–332
Fan J J, Li C, Xie C M, Liu Y M. 2016. Depositional environment and provenance of the upper Permian-Lower Triassic Tianquanshan Formation, northern Tibet: Implications for the Palaeozoic evolution of the Southern Qiangtang, Lhasa, and Himalayan terranes in the Tibetan Plateau. Int Geol Rev, 58: 228–245
Forsyth D, Uyedaf S. 1975. On the relative importance of the driving forces of plate motion. Geophys J Int, 43: 163–200
French S W, Romanowicz B A. 2014. Whole-mantle radially anisotropic shear velocity structure from spectral-element waveform tomography. Geophys J Int, 199: 1303–1327
French S W, Romanowicz B. 2015. Broad plumes rooted at the base of the Earth’s mantle beneath major hotspots. Nature, 525: 95–99
Furman T, Bryce J, Rooney T, Hanan B, Yirgu G, Ayalew D. 2006. Heads and tails: 30 million years of the Afar plume. Geol Soc London Spec Publ, 259: 95–119
Gerya T V, Stern R J, Baes M, Sobolev S V, Whattam S A. 2015. Plate tectonics on the Earth triggered by plume-induced subduction initiation. Nature, 527: 221–225
Glišović P, Forte A M. 2017. On the deep-mantle origin of the Deccan Traps. Science, 355: 613–616
Guillot S, Hattori K, Agard P, Schwartz S, Vidal O. 2009. Exhumation processes in oceanic and continental subduction contexts: A review. In: Lallemand S, Funiciello F, eds. Subduction Zone Geodynamics. Berlin Heidelberg: Springer. 175–205
Gutiérrez-Alonso G, Fernández-Suárez J, Weil A B, Brendan Murphy J, Damian Nance R, Corfú F, Johnston S T. 2008. Self-subduction of the Pangaean global plate. Nat Geosci, 1: 549–553
Hall R. 2002. Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: Computer-based reconstructions, model and animations. J Asian Earth Sci, 20: 353–431
Hall R. 2017. Southeast Asia: New views of the geology of the Malay archipelago. Annu Rev Earth Planet Sci, 45: 331–358
Hatzfeld D, Molnar P. 2010. Comparisons of the kinematics and deep structures of the Zagros and Himalaya and of the Iranian and Tibetan plateaus and geodynamic implications. Rev Geophys, 48: RG2005
Hoggard M J, White N, Al-Attar D. 2016. Global dynamic topography observations reveal limited influence of large-scale mantle flow. Nat Geosci, 9: 456–463
Hu X, Garzanti E, Wang J, Huang W, An W, Webb A. 2016. The timing of India-Asia collision onset—Facts, theories, controversies. Earth-Sci Rev, 160: 264–299
Isozaki Y, Aoki K, Nakama T, Yanai S. 2010. New insight into a subduction-related orogen: A reappraisal of the geotectonic framework and evolution of the Japanese Islands. Gondwana Res, 18: 82–105
Ji W Q, Wu F Y, Chung S L, Li J X, Liu C Z. 2009. Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of the Gangdese batholith, southern Tibet. Chem Geol, 262: 229–245
Jolivet L, Faccenna C, Agard P, Frizon de Lamotte D, Menant A, Sternai P, Guillocheau F, Polat A. 2016. Neo-Tethys geodynamics and mantle convection: From extension to compression in Africa and a conceptual model for obduction. Can J Earth Sci, 53: 1190–1204
Kelbert A, Schultz A, Egbert G. 2009. Global electromagnetic induction constraints on transition-zone water content variations. Nature, 460: 1003–1006
Kent D V, Muttoni G. 2008. Equatorial convergence of India and early Cenozoic climate trends. Proc Natl Acad Sci USA, 105: 16065–16070
Khaksar K, Rezvannia F, Kebriaei-Zadeh M R. 2014. Stratigraphy of Vali-Abad section (Central Alborz North Iran) based on corals. J Geosci Geomat, 2: 120–124
Knesel K M, Cohen B E, Vasconcelos P M, Thiede D S. 2008. Rapid change in drift of the Australian plate records collision with Ontong Java plateau. Nature, 454: 754–757
Lapierre H. 2004. The Tethyan plume: Geochemical diversity of Middle Permian basalts from the Oman rifted margin. Lithos, 74: 167–198
Li C, Zhai Q, Dong Y, Huang X. 2006. Discovery of eclogite and its geological significance in Qiangtang area, central Tibet. Chin Sci Bull, 51: 1095–1100
Li S, Jagoutz E, Chen Y, Li Q. 2000. Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains, Central China. Geochim Cosmochim Acta, 64: 1077–1093
Li Z X, Bogdanova S V, Collins A S, Davidson A, De Waele B, Ernst R E, Fitzsimons I C W, Fuck R A, Gladkochub D P, Jacobs J, Karlstrom K E, Lu S, Natapov L M, Pease V, Pisarevsky S A, Thrane K, Vernikovsky V. 2008. Assembly, configuration, and break-up history of Rodinia: A synthesis. Precambrian Res, 160: 179–210
Li Z X, Mitchell R N, Spencer C J, Ernst R, Pisarevsky S, Kirscher U, Murphy J B. 2019. Decoding Earth’s rhythms: Modulation of supercontinent cycles by longer superocean episodes. Precambrian Res, 323: 1–5
Liao S Y, Wang D B, Tang Y, Yin F G, Cao S N, Wang L Q, Wang B D, Sun Z M. 2015. Late Paleozoic Woniusi basaltic province from Sibumasu terrane: Implications for the breakup of eastern Gondwana’s northern margin. Geol Soc Am Bull, 127: 1313–1330
Liu C Z, Chung S L, Wu F Y, Zhang C, Xu Y, Wang J G, Chen Y, Guo S. 2016. Tethyan suturing in Southeast Asia: Zircon U-Pb and Hf-O isotopic constraints from Myanmar ophiolites. Geology, 44: 311–314
Liu L, Spasojevic S, Gurnis M. 2008. Reconstructing farallon plate subduction beneath North America back to the Late Cretaceous. Science, 322: 934–938
Macdonald F A, Swanson-Hysell N L, Park Y, Lisiecki L, Jagoutz O. 2019. Arc-continent collisions in the tropics set Earth’s climate state. Science, 364: 181–184
McKenzie D P, Parker R L. 1967. The North Pacific: An example of tectonics on a sphere. Nature, 216: 1276–1280
Metcalfe I. 2011. Palaeozoic-Mesozoic history of SE Asia. Geol Soc London Spec Publ, 355: 7–35
Metcalfe I. 2017. Tectonic evolution of Sundaland. Bull Geol Soc Malaysia, 63: 27–60
Morgan W J. 1968. Rises, trenches, great faults, and crustal blocks. J Geophys Res, 73: 1959–1982
Müller R D, Sdrolias M, Gaina C, Roest W R. 2008. Age, spreading rates, and spreading asymmetry of the world’s ocean crust. Geochem Geophys Geosyst, 9: Q04006
Replumaz A, Kárason H, van der Hilst R D, Besse J, Tapponnier P. 2004. 4-D evolution of SE Asia’s mantle from geological reconstructions and seismic tomography. Earth Planet Sci Lett, 221: 103–115
Robertson A H F. 2012. Late Palaeozoic-Cenozoic tectonic development of Greece and Albania in the context of alternative reconstructions of Tethys in the Eastern Mediterranean region. Int Geol Rev, 54: 373–454
Rossetti F, Monié P, Nasrabady M, Theye T, Lucci F, Saadat M. 2017. Early Carboniferous subduction-zone metamorphism preserved within the Palaeo-Tethyan Rasht ophiolites (western Alborz, Iran). J Geol Soc, 174: 741–758
Royden L, Faccenna C. 2018. Subduction orogeny and the Late Cenozoic evolution of the Mediterranean Arcs. Annu Rev Earth Planet Sci, 46: 261–289
Scotese C. 2014. Atlas of Plate Tectonic Reconstructions (Mollweide Projection). PALEOMAP Project Paleo Atlas for Arc GIS, Volumes 1–6, Evanston, Illinois
Searle M P, Noble S R, Cottle J M, Waters D J, Mitchell A H G, Hlaing T, Horstwood M S A. 2007. Tectonic evolution of the Mogok meta-morphic belt, Burma (Myanmar) constrained by U-Th-Pb dating of metamorphic and magmatic rocks. Tectonics, 26: TC3014
Şengor A M C. 1990. Plate tectonics and orogenic research after 25 years: A Tethyan perspective. Earth Sci Rev, 27: 1-201
Shellnutt J G, Bhat G M, Brookfield M E, Jahn B M. 2011. No link between the Panjal Traps (Kashmir) and the Late Permian mass extinctions. Geophys Res Lett, 38: L19308
Spakman W, Chertova M V, van den Berg A, van Hinsbergen D J J. 2018. Puzzling features of western Mediterranean tectonics explained by slab dragging. Nat Geosci, 11: 211–216
Stampfli G M, Borel G D. 2002. A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons. Earth Planet Sci Lett, 196: 17–33
Stampfli G M, Hochard C, Vérard C, Wilhem C, vonRaumer J. 2013. The formation of Pangea. Tectonophysics, 593: 1–19
Stern R J. 2002. Subduction zones. Rev Geophys, 40: 1012
Stern R. 2004. Subduction initiation: Spontaneous and induced. Earth Planet Sci Lett, 226: 275–292
Storey B C. 1995. The role of mantle plumes in continental breakup: Case histories from Gondwanaland. Nature, 377: 301–308
Storey M, Mahoney J J, Saunders A D, Duncan R A, Kelley S P, Coffin M F. 1995. Timing of hot spot—related volcanism and the breakup of Madagascar and India. Science, 267: 852–855
Sun W, Liu L, Hu Y, Ding W, Liu J, Ling M, Ding X, Zhang Z, Sun X, Li C, Li H, Fan W. 2018. Post-ridge-subduction acceleration of the Indian plate induced by slab rollback. Solid Earth Sci, 3: 1–7
Torsvik T H, Amundsen H, Hartz E H, Corfu F, Kusznir N, Gaina C, Doubrovine P V, Steinberger B, Ashwal L D, Jamtveit B. 2013. A Precambrian microcontinent in the Indian Ocean. Nat Geosci, 6: 223–227
Torsvik T H, Burke K, Steinberger B, Webb S J, Ashwal L D. 2010. Diamonds sampled by plumes from the core-mantle boundary. Nature, 466: 352–355
Torsvik T H, Cocks L R M. 2017. Earth History and Palaeogeography. Cambridge: Cambridge University Press. 317
Torsvik T H, Müller R D, Van der Voo R, Steinberger B, Gaina C. 2008. Global plate motion frames: Toward a unified model. Rev Geophys, 46: RG3004
Torsvik T H, van der Voo R, Doubrovine P V, Burke K, Steinberger B, Ashwal L D, Trønnes R G, Webb S J, Bull A L. 2014. Deep mantle structure as a reference frame for movements in and on the Earth. Proc Natl Acad Sci USA, 111: 8735–8740
Touret J L R, Huizenga J M. 2012. Fluid-assisted granulite metamorphism: A continental journey. Gondwana Res, 21: 224–235
Vaes B, van Hinsbergen D J J, Boschman L M. 2019. Reconstruction of subduction and back-arc spreading in the NW Pacific and Aleutian Basin: Clues to causes of Cretaceous and Eocene plate reorganizations. Tectonics, 38: 1367–1413
van der Meer D G, van Hinsbergen D J J, Spakman W. 2018. Atlas of the underworld: Slab remnants in the mantle, their sinking history, and a new outlook on lower mantle viscosity. Tectonophysics, 723: 309–448
van Hinsbergen D J J, Hafkenscheid E, Spakman W, Meulenkamp J E, Wortel R. 2005. Nappe stacking resulting from subduction of oceanic and continental lithosphere below Greece. Geology, 33: 325–328
Hinsbergen D J J, Steinberger B, Doubrovine P V, Gassmöller R. 2011. Acceleration and deceleration of India-Asia convergence since the Cretaceous: Roles of mantle plumes and continental collision. J Geophys Res, 116: B06101
Wan B, Xiao W, Windley B F, Yuan C. 2013. Permian hornblende gabbros in the Chinese Altai from a subduction-related hydrous parent magma, not from the Tarim mantle plume. Lithosphere, 5: 290–299
White R, McKenzie D. 1989. Magmatism at rift zones: The generation of volcanic continental margins and flood basalts. J Geophys Res, 94: 7685–7729
Wilson J T. 1966. Did the Atlantic close and then re-open? Nature, 211: 676–681
Xiao W J, Windley B F, Chen H L, Zhang G C, Li J L. 2002. Carboniferous-Triassic subduction and accretion in the western Kunlun, China: Implications for the collisional and accretionary tectonics of the northern Tibetan Plateau. Geology, 30: 295–298
Xu Z, Zheng Y F. 2017. Continental basalts record the crust-mantle interaction in oceanic subduction channel: A geochemical case study from eastern China. J Asian Earth Sci, 145: 233–259
Yin A. 2010. Cenozoic tectonic evolution of Asia: A preliminary synthesis. Tectonophysics, 488: 293–325
Yin A, Harrison T M. 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annu Rev Earth Planet Sci, 28: 211–280
Yoshida M. 2016. Formation of a future supercontinent through plate motion-driven flow coupled with mantle downwelling flow. Geology, 44: 755–758
Zahirovic S, Seton M, Müller R D. 2014. The Cretaceous and Cenozoic tectonic evolution of Southeast Asia. Solid Earth, 5: 227–273
Zanchi A, Zanchetta S, Balini M, Ghassemi M R. 2016. Oblique convergence during the Cimmerian collision: Evidence from the Triassic Aghdarband Basin, NE Iran. Gondwana Res, 38: 149–170
Zhai Q, Jahn B, Su L, Ernst R E, Wang K, Zhang R, Wang J, Tang S. 2013. SHRIMP zircon U-Pb geochronology, geochemistry and Sr-Nd-Hf isotopic compositions of a mafic dyke swarm in the Qiangtang terrane, northern Tibet and geodynamic implications. Lithos, 174: 28–43
Zhang N, Dang Z, Huang C, Li Z X. 2018. The dominant driving force for supercontinent breakup: Plume push or subduction retreat? Geosci Front, 9: 997–1007
Zhang R Y, Lo C H, Chung S L, Grove M, Omori S, Iizuka Y, Liou J G, Tri T V. 2013. Origin and tectonic implication of ophiolite and eclogite in the Song Ma Suture Zone between the South China and Indochina blocks. J Metamorph Geol, 31: 49–62
Zhang Z, Zhao G, Santosh M, Wang J, Dong X, Shen K. 2010. Late Cretaceous charnockite with adakitic affinities from the Gangdese batholith, southeastern Tibet: Evidence for Neo-Tethyan mid-ocean ridge subduction? Gondwana Res, 17: 615–631
Zheng Y, Xu Z, Zhao Z, Dai L. 2018. Mesozoic mafic magmatism in North China: Implications for thinning and destruction of cratonic lithosphere. Sci China Earth Sci, 61: 353–385
Zheng Y F. 2012. Metamorphic chemical geodynamics in continental subduction zones. Chem Geol, 328: 5–48
Zheng Y F, Chen R X. 2017. Regional metamorphism at extreme conditions: Implications for orogeny at convergent plate margins. J Asian Earth Sci, 145: 46–73
Zheng Y F, Chen Y X. 2016. Continental versus oceanic subduction zones. Natl Sci Rev, 3: 495–519
Zheng Y, Mao J, Chen Y, Sun W, Ni P, Yang X. 2019. Hydrothermal ore deposits in collisional orogens. Sci Bull, 64: 205–212
Zheng Y, Wu F. 2018. The timing of continental collision between India and Asia. Sci Bull, 63: 1649–1654
Zheng Y F, Zhao Z F. 2017. Introduction to the structures and processes of subduction zones. J Asian Earth Sci, 145: 1–15
Zhu D C, Wang Q, Cawood P A, Zhao Z D, Mo X X. 2017. Raising the Gangdese Mountains in southern Tibet. J Geophys Res-Solid Earth, 122: 214–223
Zhu D C, Zhao Z D, Niu Y, Mo X X, Chung S L, Hou Z Q, Wang L Q, Wu F Y. 2011. The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth. Earth Planet Sci Lett, 301: 241–255
Acknowledgements
We thank Ting Yang for the help on constructing dynamic topography and Anna Kelbert for providing the data for global electromagnetic induction. We appreciate fruitful discussions with participants in the “2018 Tethyan dynamics” workshop in Beijing. We thank Douwe van Hinsbergen and Zhonghai Li for critical comments and editors Lijun Liu and Yongfei Zheng for constructive suggestions, which improve our manuscript. We finally thank the inspiring talks with many colleagues over the years in Coffice 442 in IGGCAS. This study was supported by the National Natural Science Foundation of China (Grant Nos. 91855207, 41888101) and the Programs of the Chinese Academy of Sciences (Grant Nos. 2013047, GJHZ1776).
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Wan, B., Wu, F., Chen, L. et al. Cyclical one-way continental rupture-drift in the Tethyan evolution: Subduction-driven plate tectonics. Sci. China Earth Sci. 62, 2005–2016 (2019). https://doi.org/10.1007/s11430-019-9393-4
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DOI: https://doi.org/10.1007/s11430-019-9393-4