Eohimalayan metamorphism and subsequent tectonic quiescence explained
Earth and Planetary Science Letters(2022)
摘要
•Numerical model results provide explanations for Eohimalayan orogenesis.•Models show opening of Neotethys subduction channel and asthenospheric upwelling.•Upwelling heats Himalayan crust producing Early Eohimalayan 52-45 Ma metamorphism.•Mantle delamination leads to passive Indian northward motion and 45-30 Ma quiescence.•Radioactive heating assists metamorphism during Late Eohimalayan tectonic quiescence.
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关键词
Himalayan tectonics,geodynamic modeling,subduction channel opening,early Eohimalayan metamorphism,late Eohimalayan tectonic quiescence
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