Origin and composition of three heterolithic boulder- and cobble-bearing deposits overlying the Murray and Stimson formations, Gale Crater, Mars

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Date
2020-06-06
Authors
Wiens, Roger
Edgett, Kenneth S.
Stack, Kathryn M.
Dietrich, William E.
Bryk, Alexander B.
Mangold, Nicolas
Bedford, Candice
https://orcid.org/0000-0002-0783-1064
Gasda, Patrick J.
Fairén, Alberto G.
Journal Title
Journal ISSN
Volume Title
Publisher
Elsevier
Abstract
Here we present ground-based observations regarding a puzzling type of geological unit first observed prior to landing. Using ~25 cm/pixel High Resolution Imaging Science Experiment (HiRISE; McEwen et al., 2007) images acquired from the orbiting Mars Reconnaissance Orbiter (MRO), the team identified a suite of isolated features ranging in size from 10s to 100s of meters across that occur along the lower northern slopes of Aeolis Mons (informally, Mt. Sharp), the 5-km-high stratified mountain in Gale (Fig. 1). The strata of Aeolis Mons are sedimentary (Malin and Edgett, 2000; Anderson and Bell, 2010; Milliken et al., 2010). The puzzle was whether these isolated features are part of the sedimentary rock record (i.e., lithified units) or are younger, unconsolidated deposits.
Description
Keywords
Mars (Planet)--Geology
Citation
R.C. Wiens, K.S. Edgett, K.M. Stack, et al., Origin and composition of three heterolithic boulder and cobble bearing deposits overlying the Murray and Stimson formations, Gale Crater, Mars, Icarus (2020), https://doi.org/10.1016/j.icarus.2020.113897 This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain.