ArticleJournal of geophysical research. Planets2022
From Lake to River: Documenting an Environmental Transition Across the Jura/Knockfarril Hill Members Boundary in the Glen Torridon Region of Gale Crater (Mars).
Article in Journal of geophysical research. Planets, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.
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Who cites it
7 citing papers in PubMed.
- Diverse organic molecules on Mars revealed by the first SAM TMAH experiment.Nature communications · 2026Article
- Wave ripples formed in ancient, ice-free lakes in Gale crater, Mars.Science advances · 2025Article
- Diagenesis of the Clay-Sulfate Stratigraphic Transition, Mount Sharp Group, Gale Crater, Mars.Journal of geophysical research. Planets · 2024Article
- Lacustrine sedimentation by powerful storm waves in Gale crater and its implications for a warming episode on Mars.Scientific reports · 2023Article
- The Curiosity Rover's Exploration of Glen Torridon, Gale Crater, Mars: An Overview of the Campaign and Scientific Results.Journal of geophysical research. Planets · 2023Article
- From Lake to River: Documenting an Environmental Transition Across the Jura/Knockfarril Hill Members Boundary in the Glen Torridon Region of Gale Crater (Mars).Journal of geophysical research. Planets · 2022Article
- Orbital and In-Situ Investigation of Periodic Bedrock Ridges in Glen Torridon, Gale Crater, Mars.Journal of geophysical research. Planets · 2022Article
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17 authors.
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No grant is acknowledged in the PubMed record.
Abstract
Between January 2019 and January 2021, the Mars Science Laboratory team explored the Glen Torridon (GT) region in Gale crater (Mars), known for its orbital detection of clay minerals. Mastcam, Mars Hand Lens Imager, and ChemCam data are used in an integrated sedimentological and geochemical study to characterize the Jura member of the upper Murray formation and the Knockfarril Hill member of the overlying Carolyn Shoemaker formation in northern GT. The studied strata show a progressive transition represented by interfingering beds of fine-grained, recessive mudstones of the Jura member and coarser-grained, cross-stratified sandstones attributed to the Knockfarril Hill member. Whereas the former are interpreted as lacustrine deposits, the latter are interpreted as predominantly fluvial deposits. The geochemical composition seen by the ChemCam instrument show K
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