
Supporting information for the manuscript: “Fast and spatially heterogeneous cooling rates at amphibolite-facies conditions reveal the significance of local heat sources: a case study from the Lepontine Alps (Switzerland)” by Tagliaferri, A., Moulas, E., Schmalholz, S. M., & Schenker, F. L. Submitted to Geochemistry, Geophysics, Geosystems.
Diffusion geospeedometry, Garnet multicomponent diffusion modelling, Cooling rate estimation, Barrovian metamorphism, Shear heating, Ductile shear zone
Diffusion geospeedometry, Garnet multicomponent diffusion modelling, Cooling rate estimation, Barrovian metamorphism, Shear heating, Ductile shear zone
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