Search results for "Sulfate minerals"

showing 4 items of 4 documents

Sulfate deposition in subsurface regolith in Gusev crater, Mars

2006

Excavating into the shallow Martian subsurface has the potential to expose stratigraphic layers and mature regolith, which may hold a record of more ancient aqueous interactions than those expected under current Martian surface conditions. During the Spirit rover's exploration of Gusev crater, rover wheels were used to dig three trenches into the subsurface regolith down to 6-11 cm depth: Road Cut, the Big Hole, and The Boroughs. A high oxidation state of Fe and high concentrations of Mg, S, Cl, and Br were found in the subsurface regolith within the two trenches on the plains, between the Bonneville crater and the foot of Columbia Hills. Data analyses on the basis of geochemistry and miner…

Atmospheric ScienceGeochemistrySoil ScienceMineralogyAquatic Scienceengineering.materialOceanographychemistry.chemical_compoundImpact craterKieseriteGeochemistry and PetrologyMartian surfaceEarth and Planetary Sciences (miscellaneous)SulfateEjectaEarth-Surface ProcessesWater Science and TechnologyMartianEcologyPaleontologyForestryRegolithGeophysicschemistrySpace and Planetary ScienceengineeringSulfate mineralsGeologyJournal of Geophysical Research: Planets
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In-situ Mössbauer Spectroscopy with MIMOS II at Rio Tinto, Spain

2010

The Rio Tinto, located in southwest Spain, exhibits a nearly constant, acidic pHvalue along its course. Due to the formation of sulfate minerals, Rio Tinto is considered a potential analogue site for sulfate-rich regions on Mars, in particular at the landing site of the Mars Exploration Rover Opportunity, where the ferric sulfate mineral jarosite was identified with Opportunity's Mössbauer spectrometer. Primary and secondary mineralogy was investigated in situ with portable Raman and Mössbauer spectrometers at four different Rio Tinto sampling sites. The two techniques analyse different sample portions due to their specific field of view and sampling depth and provide complementar…

In situHistoryMineralMineralogyMars Exploration ProgramSampling depthengineering.materialComputer Science ApplicationsEducationchemistry.chemical_compoundchemistryMössbauer spectroscopyJarositeengineeringSulfate mineralsSulfategeographic locationsGeology
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Impact of hydrothermal alteration processes on element mobility and potential environmental implications at the Sousaki solfataric field (Corinthia -…

2020

Abstract Samples of efflorescences and encrustations of hydrothermal origin were collected at Sousaki (Greece) and analysed for their mineralogical (XRD) and chemical composition. Solutions obtained both from mineralization with HNO3 and from leaching with deionised water were analysed for major (ICP-OES), minor and trace metals (ICP-MS) and sulfate contents (IC). Results evidence the dependence of the chemical and mineralogical composition on micro-environmental conditions i.e. humidity, oxygen-rich or -poor environment, exposed or sheltered from meteoric agents. In fact, the presence of highly soluble sulfate minerals with elevated contents of many metals (e.g. Mg, Al, Fe, Mn, Cr, Ni, etc…

Mineralization (geology)010504 meteorology & atmospheric sciencesElements' mobility Hydrothermal alteration products Sulfates Toxic metalsHumidity010502 geochemistry & geophysics01 natural sciencesMineralogical compositionHydrothermal circulationchemistry.chemical_compoundGeophysicschemistryGeochemistry and PetrologyEnvironmental chemistrySulfate mineralsSulfateChemical compositionGeology0105 earth and related environmental sciences
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Potentially harmfull elements accumulation in fumarolic alteration products at three hydrothermal systems of Greece

2018

Samples of efflorescences and encrustations of hydrothermal origin have been collected at three fumarolic areas in Greece. The three sites are Sousaki, Thiafi (Methana) and Kokkino Nero (Kos) and all belong to the South Aegean Active Volcanic Arc. Samples were analysed for their mineralogical (XRD and SEM-EDS) and chemical composition. Solutions obtained from both mineralization with HNO3 and leaching with distilled water, were analysed for major (ICP-OES), minor and trace metals (ICP-MS) and for sulfate contents (IC). Results show that their composition is mainly controlled by the petrological composition of the substrate (ultramafic rocks at Sousaki, felsic volcanic rocks at Methana and l…

Settore GEO/06 - Mineralogiaefflorescences Greece sulfate mineralsSettore GEO/08 - Geochimica E Vulcanologia
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