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Evidence for a Diagenetic Origin of Vera Rubin Ridge, Gale Crater, Mars: Summary and Synthesis of Curiosity 's Exploration Campaign

Title: Evidence for a Diagenetic Origin of Vera Rubin Ridge, Gale Crater, Mars: Summary and Synthesis of Curiosity 's Exploration Campaign
Authors: Fraeman, A, A; Edgar, L, A; Rampe, E, B; Thompson, L, M; Frydenvang, J; Fedo, C, M; Catalano, J, G; Dietrich, W, E; Gabriel, T, S J; Vasavada, A, R; Grotzinger, J, P; L'Haridon, J; Mangold, N.; Sun, V, Z; House, C, H; Bryk, A, B; Hardgrove, C; Czarnecki, S; Stack, K, M; Morris, R, V; Arvidson, R, E; Banham, S, G; Bennett, K, A; Bridges, J, C; Edwards, C, S; Fischer, W, W; Fox, V, K; Gupta, S; Horgan, B, H N; Jacob, S, R; Johnson, J, R; Johnson, S, S; Rubin, D, M; Salvatore, M, R; Schwenzer, S, P; Siebach, K, L; Stein, N, T; Turner, S, M R; Wellington, D, F; Wiens, R, C; Williams, A, J; David, G; Wong, G, M
Contributors: Jet Propulsion Laboratory (JPL); NASA-California Institute of Technology (CALTECH); Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG); Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST); Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS); Institut de recherche en astrophysique et planétologie (IRAP); Université Toulouse III - Paul Sabatier (UT3); Communauté d'universités et établissements de Toulouse (Comue de Toulouse)-Communauté d'universités et établissements de Toulouse (Comue de Toulouse)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS); ANR-16-IDEX-0007,NExT (I-SITE),NExT (I-SITE)(2016)
Source: ISSN: 2169-9097.
Publisher Information: CCSD; Wiley-Blackwell
Publication Year: 2020
Collection: Université Toulouse III - Paul Sabatier: HAL-UPS
Subject Terms: [SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
Description: International audience ; This paper provides an overview of the Curiosity rover's exploration at Vera Rubin ridge (VRR) and summarizes the science results. VRR is a distinct geomorphic feature on lower Aeolis Mons (informally known as Mount Sharp) that was identified in orbital data based on its distinct texture, topographic expression, and association with a hematite spectral signature. Curiosity conducted extensive remote sensing observations, acquired data on dozens of contact science targets, and drilled three outcrop samples from the ridge, as well as one outcrop sample immediately below the ridge. Our observations indicate that strata composing VRR were deposited in a predominantly lacustrine setting and are part of the Murray formation. The rocks within the ridge are chemically in family with underlying Murray formation strata. Red hematite is dispersed throughout much of the VRR bedrock, and this is the source of the orbital spectral detection. Gray hematite is also present in isolated, gray‐colored patches concentrated toward the upper elevations of VRR, and these gray patches also contain small, dark Fe‐rich nodules. We propose that VRR formed when diagenetic event(s) preferentially hardened rocks, which were subsequently eroded into a ridge by wind. Diagenesis also led to enhanced crystallization and/or cementation that deepened the ferric‐related spectral absorptions on the ridge, which helped make them readily distinguishable from orbit. Results add to existing evidence of protracted aqueous environments at Gale crater and give new insight into how diagenesis shaped Mars' rock record.
Document Type: article in journal/newspaper
Language: English
DOI: 10.1029/2020je006527
Availability: https://hal.science/hal-03104157; https://hal.science/hal-03104157v1/document; https://hal.science/hal-03104157v1/file/P186_Fraeman-JGR-2020.pdf; https://doi.org/10.1029/2020je006527
Rights: info:eu-repo/semantics/OpenAccess
Accession Number: edsbas.9346FB5F
Database: BASE