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Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

From: Sensitivity of elastic thickness to water in the Martian lithosphere

Fig. 6

Rheological structures of the Martian lithosphere at Pavonis Mons, Alba Patera, and NE Arabia Terra calculated under dry (a) and wet (b) conditions. The plastic strength changes across the crust-mantle boundary (Moho) due to a change in flow laws. Elastic thickness was calculated from the integrated bending moment within the lithosphere (see text for details)

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