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      The first X-ray diffraction measurements on Mars

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          Abstract

          The Mars Science Laboratory landed in Gale crater on Mars in August 2012, and the Curiosity rover then began field studies on its drive toward Mount Sharp, a central peak made of ancient sediments. CheMin is one of ten instruments on or inside the rover, all designed to provide detailed information on the rocks, soils and atmosphere in this region. CheMin is a miniaturized X-ray diffraction/X-ray fluorescence (XRD/XRF) instrument that uses transmission geometry with an energy-discriminating CCD detector. CheMin uses onboard standards for XRD and XRF calibration, and beryl:quartz mixtures constitute the primary XRD standards. Four samples have been analysed by CheMin, namely a soil sample, two samples drilled from mudstones and a sample drilled from a sandstone. Rietveld and full-pattern analysis of the XRD data reveal a complex mineralogy, with contributions from parent igneous rocks, amorphous components and several minerals relating to aqueous alteration. In particular, the mudstone samples all contain one or more phyllosilicates consistent with alteration in liquid water. In addition to quantitative mineralogy, Rietveld refinements also provide unit-cell parameters for the major phases, which can be used to infer the chemical compositions of individual minerals and, by difference, the composition of the amorphous component.

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          Most cited references13

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          Two-dimensional detector software: From real detector to idealised image or two-theta scan

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            A habitable fluvio-lacustrine environment at Yellowknife Bay, Gale crater, Mars.

            The Curiosity rover discovered fine-grained sedimentary rocks, which are inferred to represent an ancient lake and preserve evidence of an environment that would have been suited to support a martian biosphere founded on chemolithoautotrophy. This aqueous environment was characterized by neutral pH, low salinity, and variable redox states of both iron and sulfur species. Carbon, hydrogen, oxygen, sulfur, nitrogen, and phosphorus were measured directly as key biogenic elements; by inference, phosphorus is assumed to have been available. The environment probably had a minimum duration of hundreds to tens of thousands of years. These results highlight the biological viability of fluvial-lacustrine environments in the post-Noachian history of Mars.
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              Mars Science Laboratory Mission and Science Investigation

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                Author and article information

                Journal
                IUCRAJ
                IUCrJ
                IUCrJ
                IUCr J
                Int Union Crystallogr J
                Int Union Cryst J
                International Union of Crystallography (IUCr)
                2052-2525
                November 2014
                October 21 2014
                November 01 2014
                : 1
                : 6
                : 514-522
                Article
                10.1107/S2052252514021150
                8fe62f63-235d-4235-bb43-12c4f4fe20d7
                © 2014

                http://creativecommons.org/licenses/by/2.0/uk/legalcode

                http://creativecommons.org/licenses/by/2.0/uk/legalcode

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