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Supplemental Material: Subduction polarity reversal facilitated by plate coupling during arc-continent collision: Evidence from the Western Kunlun orogenic belt, northwest Tibetan Plateau

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posted on 2024-01-24, 20:56 authored by Zaili Tao, Jiyuan Yin, W.J. Xiao, et al.

Materials and methods, Figures S1–S6, and Tables S1–S7.  

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    Geology

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    Keywords

    Subduction polarity reversalarc-continent collisionProto-Tethys OceanPlate couplingTemporal-spatial variation

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    CC BY-NC 4.0

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