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gouges that weaken the fault and decrease its core permeability over time. Such a process could also deteriorate the flow properties in Enhanced Geothermal Reservoirs, such as Alsace, which is also a place
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with the LEGI, IMFT and ISAE-SUPAERO laboratories, it is proposed to model the dynamics of cryogenic fluids at the reservoir scale by integrating sub-models from direct numerical simulations developed by
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supposedly pond above magmatic reservoirs at 1-6 km depth beneath active volcanoes. These fluids are believed to source Cu-Au-Mo porphyry ore deposits in arc-settings and may act as filters modifying
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