Heat flux and temperature at depth beneath InSight landing site through time

Szilard Gyalay, Francis Nimmo, Ana-Catalina Plesa & Mark Wieczorek
The heat flux and thus temperature gradient of the Martian crust is critical for comparison with measurements of crustal properties. This allows for constraints upon the inferred thermal history of Mars. Each file contains the heat flux and temperature at several depths as a function of time after Mars formed, but assuming different crustal properties.
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