Using 3D reconstructions of centimeter-scale sedimentary structures to document changes in the depositional settings of Glen Torridon region (Gale crater, Mars)
Résumé
The Glen Torridon (GT) region in Gale crater, has been explored using the Mars Science Laboratory rover, Curiosity, since January 2019 (~Sol 2300) to document clay-bearing rocks initially detected via orbiter data [1]. The rocks are part of the Murray formation, with lower GT consisting of the Jura member mudstones generally associated with a lacustrine deposition [2] overlain by laminated and cross-bedded fine-grained sandstones of the Knockfarril Hill (KfH) member. The latter hint at a sharp change in depositional environment that is critical to investigate [2]. To that extent, we use high-resolution photogrammetric micro-Digital Outcrop Models (DOM) to characterize centimeter-scale sedimentary structures in the KfH member to shed light on their implications in terms of depositional settings and dynamics.
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