Linking Cenozoic Magmatism in the North‐Central Tibetan Plateau With Plateau Growth

AGU Publications·Apr 7

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Research is exploring the connection between Cenozoic magmatism and the growth of the north-central Tibetan Plateau. Studies are investigating various mechanisms, including uplift, subduction, and deformation, that have contributed to the plateau's development. The findings suggest a complex and multi-stage process, with different factors influencing the plateau's growth at different times and locations.

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The Cenozoic Multiple-Stage Uplift of the Qiangtang Terrane, Tibetan Plateau

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Science | AAAS·Jul 7

Late Eocene to Oligocene intracontinental deformation and growth of the northwestern Tibetan Plateau

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Uplift of the Tibetan Plateau driven by mantle delamination from the overriding plate

Nature·Jul 2

Eocene Rotation of the Northeastern Central Tibetan Plateau Indicating Stepwise Compressions and Eastward Extrusions

AGU Publications·Sep 2

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