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</script>Two-dimensional thermal modeling of the subduction and exhumation of the ultrahigh-pressure (UHP) Maksyutov Complex in the south Ural Mountains tests factors influencing the low modern heat flow in the Urals and the feeble preservation of UHP index minerals. Best-fit models are obtained with initial surface heat flow of 60 mW m
Thermal modeling, U-Pb SHRIMP dating of zircon, Ural Mountains, Ultrahigh-pressure metamorphism
Thermal modeling, U-Pb SHRIMP dating of zircon, Ural Mountains, Ultrahigh-pressure metamorphism
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