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A note on latent heat release from disequilibrium phase transformations and deep seismogenesis

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Figure

Fig. 1.Temperature as a function of pressure for a portion of a litho-spheric slab subducting along an adiabat that is refracted by an equilib-rium exothermic phase transition (solid)
Fig. 2.Temperature as a function of pressure for a portion of a litho-spheric slab subducting along an adiabat that is refracted by multipleequilibrium phase transitions (solid)
Fig. 4.Temperature as a function of pressure for a portion of a litho-spheric slab subducting along an adiabat that is refracted by an equilib-rium exothermic phase transition (solid)

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