Fluids during diagenesis and sulfate vein formation in sediments at Gale crater, Mars

We model the fluids involved in the alteration processes recorded in the Sheepbed Member mudstones of Yellowknife Bay (YKB), Gale crater, Mars, as revealed by the Mars Science Laboratory Curiosity rover investigations. We compare the Gale crater waters with fluids modeled for shergottites, nakhlites...

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Bibliographic Details
Published in:Meteoritics & Planetary Science
Main Authors: Schwenzer, Susanne Petra, orcid:0000-0002-9608-0759, Treiman, Allan H., orcid:0000-0002-8073-2839
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
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Online Access:https://hdl.handle.net/20.500.11753/1500
https://doi.org/10.1111/maps.12668
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Summary:We model the fluids involved in the alteration processes recorded in the Sheepbed Member mudstones of Yellowknife Bay (YKB), Gale crater, Mars, as revealed by the Mars Science Laboratory Curiosity rover investigations. We compare the Gale crater waters with fluids modeled for shergottites, nakhlites, and the ancient meteorite ALH 84001, as well as rocks analyzed by the Mars Exploration rovers, and with terrestrial ground and surface waters. S. P. Schwenzer, J. C. Bridges, R. C. Wiens, P. G. Conrad, S. P. Kelley, R. Leveille, N. Mangold, J. Martín-Torres, A. Mcadam, H. Newsom, M. P. Zorzano, W. Rapin, J. Spray, A. H. Treiman, F. Westall, A. G. Fairén, and P.-Y. Meslin