291-5 In-Situ Mineralogy of the Orbitally Defined Clay- and Sulfate-Bearing Units in Gale Crater, Mars

Session: Mineralogy in the Solar System

Presenting Author:

Elizabeth Rampe

Authors:

Rampe, Elizabeth¹, Bristow, Thomas F.², Blake, David³, Chipera, Steve⁴, Vaniman, David⁵, Grotzinger, John⁶, Peretyazhko, Tanya⁷, Simpson, Sarah⁸, Berger, Jeff⁹, O'Connell-Cooper, Catherine¹⁰, Yen, Albert¹¹, Sheppard, Rachel¹², Szczerba, Marek¹³, Treiman, Allan¹⁴, Tutolo, Benjamin¹⁵, Downs, Robert¹⁶

(1) National Aeronautics and Space Administration, Houston, TX, , (2) NASA Ames Research Center, Moffett Field, CA, , (3) NASA Ames Research Center, ; University of Hawaii, , (4) PSI, , (5) PSI, , (6) Caltech, , (7) Amentum at NASA JSC, , (8) Amentum at NASA JSC, , (9) Amentum at NASA JSC, , (10) University of New Brunswick, , (11) PSI, , (12) PSI, , (13) Polish Academy of Sciences, , (14) Lunar and Planetary Institute, , (15) University of Calgary, , (16) University of Arizona, , (17) Rutgers University, , (18) University of Cambridge, , (19) NASA Johnson Space Center, , (20) NASA Johnson Space Center, , (21) Amentum at NASA JSC, , (22) NASA Goddard Space Flight Center, ; University of Maryland, , (23) Interlune, , (24) NASA Ames Research Center, , (25) Carnegie Institution for Science, ,

Abstract:

Gale crater was selected as the Mars Science Laboratory Curiosity rover’s landing site, in part, because of orbital detection of secondary minerals in ~3.5 Ga sedimentary rocks. Secondary minerals include Fe/Mg-smectite, hydrated Mg-sulfate, and hematite. The observed transition from clay minerals to hydrated Mg-sulfate going up stratigraphic section through the Mount Sharp Group was interpreted to signify a change in climate that may have occurred across Mars. The CheMin X-ray diffractometer on Curiosity has analyzed dozens of drill samples from units with secondary mineral absorptions from orbit. Quantitative mineralogical results from CheMin demonstrate spatially abrupt changes in mineral assemblages that may be from variations in depositional, early diagenetic, and late diagenetic environments. We hypothesize that smectite is a marker of fluvial-lacustrine depositional environments and that Fe(II)-carbonate, hydrated Mg-sulfate, gypsum, and halite represent early diagenetic products of near-surface groundwater freezing/evaporation in eolian environments. We present a late-diagenetic groundwater mixing model in which warm, oxic and acidic basinal brines ascended through fluvial-lacustrine and some eolian strata to cause the formation of Fe(III)-oxides, -oxyhydroxides, and -smectite and mobilization of transition metals. These warm brines mixed with cool, reducing groundwater at a local aquiclude called the Amapari Marker Band, causing high concentrations of Fe, Zn, and Cl.

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