Analysis of tracking data from Mars orbiters reveals time-variable gravity field behaviour reflecting the structure underlying the Martian crustal dichotomy and indicates the preservation of a 200–400 °C thermal anomaly in the present-day mantle below the southern highlands.

Analysis of tracking data from Mars orbiters reveals time-variable gravity field behaviour reflecting the structure underlying the Martian crustal dichotomy and indicates the…

Scientists have used a novel technique to detect a major temperature asymmetry under the surface of Mars that could shed light on the evolution and past habitability of the red…