Thermal Modeling of Permafrost Melt by Overlying Lava Flows with Applications to Flow-associated Outflow Channel Volumes in the Cerberus Plains, Mars

Physics

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Scientific paper

Heat from observed lava flow thicknesses near an E. Cerberus region vent
is modeled to determine if thermal pulses into the substrate can melt
pore space ice sufficient to fill local small spatially related fluvial
channel networks.

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