0000000000749604

AUTHOR

P. Bartlett

showing 2 related works from this author

Characterization and petrologic interpretation of olivine-rich basalts at Gusev Crater, Mars

2006

Rocks on the floor of Gusev crater are basalts of uniform composition and mineralogy. Olivine, the only mineral to have been identified or inferred from data by all instruments on the Spirit rover, is especially abundant in these rocks. These picritic basalts are similar in many respects to certain Martian meteorites (olivine-phyric shergottites). The olivine megacrysts in both have intermediate compositions, with modal abundances ranging up to 20-30%. Associated minerals in both include low-calcium and high-calcium pyroxenes, plagioclase of intermediate composition, iron-titanium-chromium oxides, and phosphate. These rocks also share minor element trends, reflected in their nickel-magnesiu…

Atmospheric ScienceGeochemistrySoil SciencePyroxeneAquatic Scienceengineering.materialOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)PlagioclaseIntermediate compositionAchondriteEarth-Surface ProcessesWater Science and TechnologyBasaltgeographyOlivinegeography.geographical_feature_categoryEcologyPaleontologyForestryVolcanic rockIgneous rockGeophysicsSpace and Planetary ScienceengineeringGeologyJournal of Geophysical Research: Planets
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Search for magnetic minerals in Martian rocks: Overview of the Rock Abrasion Tool (RAT) magnet investigation on Spirit and Opportunity

2008

[1] The Rock Abrasion Tool (RAT) on board the Mars Exploration Rovers (MER) is a grinding tool designed to remove dust coatings and/or weathering rinds from rocks and expose fresh rock material. Four magnets of different strengths that are built into the structure of the RAT have been attracting substantial amounts of magnetic material during RAT activities from rocks throughout both rover missions. The RAT magnet experiment as performed on Spirit demonstrates the presence of a strongly ferrimagnetic phase in Gusev crater rocks, which based on Mossbauer and visible/near-infrared reflectance spectra is interpreted as magnetite. The amount of abraded rock material adhering to the magnets vari…

MartianAtmospheric ScienceEcologyPaleontologySoil ScienceMineralogyForestryWeatheringMars Exploration ProgramAquatic ScienceOceanographyAbrasion (geology)chemistry.chemical_compoundMagnetizationGeophysicschemistryImpact craterSpace and Planetary ScienceGeochemistry and PetrologyFerrimagnetismEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyMagnetiteJournal of Geophysical Research
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