Figure F3. Schematic representation of the predictions of the general depth trends of latent heat release, bulk Mg#, strain rate, cooling rate, hydrothermal fluid flux, fluid temperature, and intensity of high-temperature (HT) alteration for the end-member “gabbro glacier” (with mainly conductive cooling of the lower crust) and “sheeted sill” (with convective cooling of the lower crust) models (from Gillis et al., 2012).
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