Abstract
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
Original language | English |
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Pages (from-to) | 85-99 |
Journal | Earth and Planetary Science Letters |
Volume | 226 |
DOIs | |
Publication status | Published - 2004 |