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Contrasting styles of water-rock interaction at the Mars Exploration Rover landing sites

Hurowitz, Joel A. and Fischer, Woodward W. (2014) Contrasting styles of water-rock interaction at the Mars Exploration Rover landing sites. Geochimica et Cosmochimica Acta, 127 . pp. 25-38. ISSN 0016-7037. https://resolver.caltech.edu/CaltechAUTHORS:20140219-080829707

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Abstract

The nature of ancient hydrological systems on Mars has been the subject of ongoing controversy, driven largely by a disconnect between observational evidence for flowing water on the Martian surface at multiple scales and the incompatibility of such observations with theoretical models that predict a cold early Martian environment in which liquid water is unstable. Here we present geochemical data from the Mars Exploration Rovers to evaluate the hydrological conditions under which weathering rinds, soils, and sedimentary rocks were formed. Our analysis indicates that the chemistry of rinds and soils document a water-limited hydrologic environment where small quantities of S-bearing fluids enter the system, interact with and chemically alter rock and soil, and precipitate secondary mineral phases at the site of alteration with little to no physical separation of primary and secondary mineral phases. In contrast, results show that the sedimentary rocks of the Burns Formation at Meridiani Planum have a chemical composition well-described as a mixture between siliciclastic sediment and sulfate-bearing salts derived from the evaporation of groundwater. We hypothesize that the former may be derived from the recently investigated Shoemaker Formation, a sequence of impact breccias that underlie the Burns Formation. This result has important implications for the style of chemical weathering and hydrology recorded by these sedimentary materials, revealing long-range transport of ions in solution in an open hydrological system that is consistent only with subsurface or overland flow of liquid water.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.gca.2013.11.021 DOIArticle
http://www.sciencedirect.com/science/article/pii/S0016703713006601PublisherArticle
ORCID:
AuthorORCID
Fischer, Woodward W.0000-0002-8836-3054
Additional Information:© 2013 Elsevier Ltd. Received 21 September 2012; accepted in revised form 17 November 2013; available online 24 November 2013. This research was carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Agency (J.A.H.). This work was supported by NASA award NNX10AM84G to J.A.H. The authors thank associate editor Penny King, Mikhail Zolotov, and two anonymous reviewers for their helpful comments, which substantially improved this manuscript. The authors thank Ken Herkenhoff (USGS) for producing the Microscopic Imager mosaics on Fig. 2, and Edwin Kite for feedback on an early draft of the manuscript.
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Funding AgencyGrant Number
NASANNX10AM84G
Record Number:CaltechAUTHORS:20140219-080829707
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140219-080829707
Official Citation:Joel A. Hurowitz, Woodward W. Fischer, Contrasting styles of water–rock interaction at the Mars Exploration Rover landing sites, Geochimica et Cosmochimica Acta, Volume 127, 15 February 2014, Pages 25-38, ISSN 0016-7037, http://dx.doi.org/10.1016/j.gca.2013.11.021. (http://www.sciencedirect.com/science/article/pii/S0016703713006601)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:43864
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:20 Feb 2014 22:38
Last Modified:03 Oct 2019 06:12

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