Contrasting Magmatic Tempos Reveal a Segmented Trans-Tethyan Subduction System

References

[1] Aitchison J C, Ali J R, Davis A M. When and where did India and Asia Collide. Journal of Geophysical Research: Solid Earth, 2007, 112(B5): B05423.

[2] Bouilhol P, Jagoutz O, Hanchar J M, et al.. Dating the India-Eurasia Collision through Arc Magmatic Records. Earth and Planetary Science Letters, 2013, 366: 163-175.

[3] Chen S, Chen Y, Guillot S, et al.. Change in Subduction Dip Angle of the Indian Continental Lithosphere Inferred from the Western Himalayan Eclogites. Frontiers in Earth Science, 2022, 9: 790999.

[4] Chen Y. Different Metamorphic Records between Subduction Initiation and Mature Subduction. Bulletin of Mineralogy, Petrology and Geochemistry, 2019, 38(3): 490-498. (in Chinese with English Abstract).

[5] Chen Y, Ye K, Wu T F, et al.. Exhumation of Oceanic Eclogites: Thermodynamic Constraints on Pressure, Temperature, Bulk Composition and Density. Journal of Metamorphic Geology, 2013, 31(5): 549-570.

[6] Chen Y, Huang F, Shi G H, et al.. Magnesium Isotope Composition of Subduction Zone Fluids as Constrained by Jadeitites from Myanmar. Journal of Geophysical Research: Solid Earth, 2018, 123(9): 7566-7585.

[7] Chen Y, Zhang Q H, Chen L, et al.. Intra-Oceanic Subduction Termination and Reinitiation of the Eastern Neo-Tethys in Myanmar. Journal of Earth Science, 2024, 35(3): 1053-1058.

[8] Duretz T, Gerya T V, Spakman W. Slab Detachment in Laterally Varying Subduction Zones: 3-D Numerical Modeling. Geophysical Research Letters, 2014, 41(6): 1951-1956.

[9] Goffé B, Rangin C, Maluski H. Jade and Associated Rocks from Jade Mines Area, Northern Myanmar as Record of a Polyphased High-Pressure Metamorphism. Eos Transactions American Geophysical Union, 2000, 81: F1365

[10] Guo S, Chu X, Hermann J, et al.. Multiple Episodes of Fluid Infiltration along a Single Metasomatic Channel in Metacarbonates (Mogok Metamorphic Belt, Myanmar) and Implications for CO₂ Release in Orogenic Belts. Journal of Geophysical Research: Solid Earth, 2021, 126(1): e2020JB020988.

[11] Gutscher M A, Spakman W, Bijwaard H, et al.. Geodynamics of Flat Subduction: Seismicity and Tomographic Constraints from the Andean Margin. Tectonics, 2000, 19(5): 814-833.

[12] Hall R. Late Jurassic–Cenozoic Reconstructions of the Indonesian Region and the Indian Ocean. Tectonophysics, 2012, 570/571: 1-41.

[13] Hamada M, Iwamori H, Brandl P A, et al.. Temporal Evolution of Proto-Izu-Bonin-Mariana Arc Volcanism over 10 Myr: Constraints from Statistical Analysis of Melt Inclusion Compositions. Journal of Petrology, 2020, 61(1): 1-29.

[14] Harlow G E, Tsujimori T, Sorensen S S. Jadeitites and Plate Tectonics. Annual Review of Earth and Planetary Sciences, 2015, 43(1): 105-138.

[15] Heuret A, Lallemand S. Plate Motions, Slab Dynamics and Back-Arc Deformation. Physics of the Earth and Planetary Interiors, 2005, 149(1/2): 31-51.

[16] Hirschmann M M. Mantle Solidus: Experimental Constraints and the Effects of Peridotite Composition. Geochemistry, Geophysics, Geosystems, 2000, 1(10): 2000GC000070.

[17] Htay H, Zaw K, Oo T T. Chapter 6: The Mafic-Ultramafic (Ophiolitic) Rocks of Myanmar. Geological Society, London, Memoirs, 2017, 48(1): 117-141.

[18] Husson L, Brun J P, Yamato P, et al.. Episodic Slab Rollback Fosters Exhumation of HP-UHP Rocks. Geophysical Journal International, 2009, 179(3): 1292-1300.

[19] Jagoutz O, Royden L, Holt A F, et al.. Anomalously Fast Convergence of India and Eurasia Caused by Double Subduction. Nature Geoscience, 2015, 8(6): 475-478.

[20] Jagoutz O, Bouilhol P, Schaltegger U, et al.. The Isotopic Evolution of the Kohistan Ladakh Arc from Subduction Initiation to Continent Arc Collision. Geological Society, London, Special Publications, 2019, 483(1): 165-182.

[21] Li J X, Fan W M, Zhang L Y, et al.. Subduction of Indian Continental Lithosphere Constrained by Eocene–Oligocene Magmatism in Northern Myanmar. Lithos, 2019, 348/349: 105211.

[22] Licht A, Win Z, Westerweel J, et al.. Magmatic History of Central Myanmar and Implications for the Evolution of the Burma Terrane. Gondwana Research, 2020, 87: 303-319.

[23] Licht A, Dupont-Nivet G, Westerweel J, et al.. The Missing Arcs of the India-Asia Collision. Gondwana Research, 2025, 147: 260-275.

[24] Lin S C. Three-Dimensional Mantle Circulations and Lateral Slab Deformation in the Southern Chilean Subduction Zone. Journal of Geophysical Research: Solid Earth, 2014, 119(4): 3879-3896.

[25] Liu C Z, Chung S L, Wu F Y, et al.. Tethyan Suturing in Southeast Asia: Zircon U-Pb and Hf-O Isotopic Constraints from Myanmar Ophiolites. Geology, 2016, 44(4): 311-314.

[26] Liu X W, Wagner L S, Currie C A, et al.. Implications of Flat-Slab Subduction on Hydration, Slab Seismicity, and Arc Volcanism in the Pampean Region of Chile and Argentina. Geochemistry, Geophysics, Geosystems, 2024, 25(3): e2023GC01131.

[27] Maibam B, Palin R M, Gerdes A, et al.. Dating Blueschist-Facies Metamorphism within the Naga Ophiolite, Northeast India, Using Sheared Carbonate Veins. International Geology Review, 2023, 65(3): 378-395.

[28] Martin C R, Jagoutz O, Upadhyay R, et al.. Paleocene Latitude of the Kohistan-Ladakh Arc Indicates Multistage India-Eurasia Collision. Proceedings of the National Academy of Sciences of the United States of America, 2020, 117(47): 29487-29494.

[29] Morley C K, Chantraprasert S, Kongchum J, et al.. The West Burma Terrane, a Review of Recent Paleo-Latitude Data, Its Geological Implications and Constraints. Earth-Science Reviews, 2021, 220: 103722.

[30] Müller R D, Zahirovic S, Williams S E, et al.. A Global Plate Model Including Lithospheric Deformation along Major Rifts and Orogens since the Triassic. Tectonics, 2019, 38(6): 1884-1907.

[31] Parsons A J, Sigloch K, Hosseini K. Australian Plate Subduction is Responsible for Northward Motion of the India-Asia Collision Zone and ∼ 1, 000 Km Lateral Migration of the Indian Slab. Geophysical Research Letters, 2021, 48(18): e2021GL094904.

[32] Qi M, Xiang H, Zhong Z Q, et al.. ⁴⁰Ar/³⁹Ar Geochronology Constraints on the Formation Age of Myanmar Jadeitite. Lithos, 2013, 162/163: 107-114.

[33] Qiu Z L, Wu F Y, Yang S F, et al.. Age and Genesis of the Myanmar Jadeite: Constraints from U-Pb Ages and Hf Isotopes of Zircon Inclusions. Chinese Science Bulletin, 2009, 54(4): 658-668.

[34] Ramos V A, Folguera A. Andean Flat-Slab Subduction through Time. Geological Society, London, Special Publications, 2009, 327(1): 31-54.

[35] Ranalli G, Martin S, Mahatsente R. Continental Subduction and Exhumation: An Example from the Ulten Unit, Tonale Nappe, Eastern Austroalpine. Geological Society, London, Special Publications, 2005, 243(1): 159-174.

[36] Schellart W P. Andean Mountain Building and Magmatic Arc Migration Driven by Subduction-Induced Whole Mantle Flow. Nature Communications, 2017, 8(1): 2010.

[37] Schmidt M W, Poli S. Experimentally Based Water Budgets for Dehydrating Slabs and Consequences for Arc Magma Generation. Earth and Planetary Science Letters, 1998, 163(1/2/3/4): 361-379.

[38] Shi G H, Cui W Y, Cao S M, et al.. Ion Microprobe Zircon U-Pb Age and Geochemistry of the Myanmar Jadeitite. Journal of the Geological Society, 2008, 165(1): 221-234.

[39] Shi G H, Harlow G E, Wang J, et al.. Mineralogy of Jadeitite and Related Rocks from Myanmar: A Review with New Data. European Journal of Mineralogy, 2012, 24(2): 345-370.

[40] Shi G H, Lei W Y, He H Y, et al.. Superimposed Tectono-Metamorphic Episodes of Jurassic and Eocene Age in the Jadeite Uplift, Myanmar, as Revealed by ⁴⁰Ar/³⁹Ar Dating. Gondwana Research, 2014, 26(2): 464-474.

[41] Singh A K, Chung S L, Bikramaditya R K, et al.. New U-Pb Zircon Ages of Plagiogranites from the Nagaland-Manipur Ophiolites, Indo-Myanmar Orogenic Belt, NE India. Journal of the Geological Society, 2017, 174(1): 170-179.

[42] Torsvik T H. Earth History: A Journey in Time and Space from Base to Top. Tectonophysics, 2019, 760: 297-313.

[43] Torsvik T H, Van der Voo R, Preeden U, et al.. Phanerozoic Polar Wander, Palaeogeography and Dynamics. Earth-Science Reviews, 2012, 114(3/4): 325-368.

[44] van Hinsbergen D J J, Steinberger B, Doubrovine P V, et al.. Acceleration and Deceleration of India-Asia Convergence since the Cretaceous: Roles of Mantle Plumes and Continental Collision. Journal of Geophysical Research: Solid Earth, 2011, 116(B6): B06101.

[45] Vogt K, Gerya T V. From Oceanic Plateaus to Allochthonous Terranes: Numerical Modelling. Gondwana Research, 2014, 25(2): 494-508.

[46] Wada I, Wang K L. Common Depth of Slab-Mantle Decoupling: Reconciling Diversity and Uniformity of Subduction Zones. Geochemistry, Geophysics, Geosystems, 2009, 10(10): Q10009.

[47] Weber J, Flament N. Factors Contributing to Slab Locations and Geometries in Reconstructions of Past Mantle Flow. Geochemistry, Geophysics, Geosystems, 2024, 25(7): e2023GC011313.

[48] Westerweel J, Roperch P, Licht A, et al.. Burma Terrane Part of the Trans-Tethyan Arc during Collision with India According to Palaeomagnetic Data. Nature Geoscience, 2019, 12(10): 863-868.

[49] Westerweel J, Roperch P, Win Z, et al.. Northward Drift of the Burma Terrane with India during the Cenozoic and Implications for the India-Asia Collision. Geological Society, London, Special Publications, 2025, 549(1): 11-54.

[50] Yan Z Y, Chen L, Xiong X, et al.. Observations and Modeling of Flat Subduction and Its Geological Effects. Science China Earth Sciences, 2020, 63(8): 1069-1091.

[51] Yang J F, Lu G, Liu T, et al.. Amagmatic Subduction Produced by Mantle Serpentinization and Oceanic Crust Delamination. Geophysical Research Letters, 2020, 47(9): e2019GL086257.

[52] Yang S, Liang X F, Jiang M M, et al.. Slab Remnants beneath the Myanmar Terrane Evidencing Double Subduction of the Neo-Tethyan Ocean. Science Advances, 2022, 8(34): eabo1027.

[53] Yang Z Y, Bi X W, Zhu J J, et al.. Mid-Cretaceous Intra-Oceanic Arc-Continent Collision Recorded by the Igneous Complex in Central Myanmar. Lithos, 2022, 414/415: 106637.

[54] Yao J H, Zhang G L, Zhang J, et al.. Petrological and Geochemical Constraints of Mantle Peridotites on the Magma-Starved Yap Arc Formed by Ultra-Slow Subduction. Contributions to Mineralogy and Petrology, 2023, 178(11): 74.

[55] Yu Y, Huang X L, Jiang Y D, et al.. Slab Structure Controls Arc Magmatism Diversity in Subduction Zones. Geological Society of America Bulletin, 2025, 137(11/12): 4649-4658.

[56] Yuan J, Deng C L, Yang Z Y, et al.. New Paleomagnetic Data from the Central Tethyan Himalaya Refine the Size of Greater India during the Campanian. Earth and Planetary Science Letters, 2023, 622: 118422.

[57] Yuan, J., Deng, C. L., Yang, Z. Y., et al., 2025. The India-Asia Collision System. National Science Review. nwaf487. https://doi.org/10.1093/nsr/nwaf487

[58] Yui T F, Fukoyama M, Iizuka Y, et al.. Is Myanmar Jadeitite of Jurassic Age? A Result from Incompletely Recrystallized Inherited Zircon. Lithos, 2013, 160: 268-282.

[59] Zahirovic S, Müller R D, Seton M, et al.. Insights on the Kinematics of the India-Eurasia Collision from Global Geodynamic Models. Geochemistry, Geophysics, Geosystems, 2012, 13(4): 2011GC003883.

[60] Zhang J E, Xiao W J, Windley B F, et al.. Early Cretaceous Wedge Extrusion in the Indo-Burma Range Accretionary Complex: Implications for the Mesozoic Subduction of Neotethys in SE Asia. International Journal of Earth Sciences, 2017, 106(4): 1391-1408.

[61] Zhang L Y, Fan W M, Ding L, et al.. Forced Subduction Initiation within the Neotethys: An Example from the Mid-Cretaceous Wuntho-Popa Arc in Myanmar. Geological Society of America Bulletin, 2022, 134(3/4): 849-870.

[62] Zhang Q H, Chen Y, Chen S, et al.. Intra-Neo-Tethyan Subduction Initiation Inferred from the Indawgyi Mafic Rocks in the Central Ophiolite Belt, Myanmar. Geological Society of America Bulletin, 2024, 136(7/8): 2753-2766.

[63] Zhang W, Zhang F Q, Dilek Y, et al.. Basin Response to the Jurassic Geodynamic Turnover from Flat Subduction to Normal Subduction in South China. Geological Society of America Bulletin, 2022, 134(7/8): 1681-1700.

[64] Zhu R X, Zhao P, Zhao L. Tectonic Evolution and Geodynamics of the Neo-Tethys Ocean. Science China Earth Sciences, 2022, 65(1): 1-24.

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