0000000000178764

AUTHOR

Morten Madsen

showing 13 related works from this author

Overview of the Spirit Mars Exploration Rover Mission to Gusev Crater: Landing site to Backstay Rock in the Columbia Hills

2006

Spirit landed on the floor of Gusev Crater and conducted initial operations on soil covered, rock-strewn cratered plains underlain by olivine-bearing basalts. Plains surface rocks are covered by wind-blown dust and show evidence for surface enrichment of soluble species as vein and void-filling materials and coatings. The surface enrichment is the result of a minor amount of transport and deposition by aqueous processes. Layered granular deposits were discovered in the Columbia Hills, with outcrops that tend to dip conformably with the topography. The granular rocks are interpreted to be volcanic ash and/or impact ejecta deposits that have been modified by aqueous fluids during and/or after…

Atmospheric ScienceOutcropGeochemistrySoil ScienceAquatic ScienceOceanographyImpact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)EjectaDust devilGeomorphologyEarth-Surface ProcessesWater Science and TechnologyBasaltgeographygeography.geographical_feature_categoryEcologyPaleontologyForestryVolcanic rockGeophysicsSpace and Planetary ScienceClastic rockGeologyVolcanic ashJournal of Geophysical Research: Planets
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The Opportunity Rover's Athena Science Investigation at Meridiani Planum, Mars

2004

The Mars Exploration Rover Opportunity has investigated the landing site in Eagle crater and the nearby plains within Meridiani Planum. The soils consist of fine-grained basaltic sand and a surface lag of hematite-rich spherules, spherule fragments, and other granules. Wind ripples are common. Underlying the thin soil layer, and exposed within small impact craters and troughs, are flat-lying sedimentary rocks. These rocks are finely laminated, are rich in sulfur, and contain abundant sulfate salts. Small-scale cross-lamination in some locations provides evidence for deposition in flowing liquid water. We interpret the rocks to be a mixture of chemical and siliciclastic sediments formed by e…

Meridiani PlanumGeologic SedimentsMineralsMultidisciplinaryExtraterrestrial EnvironmentAtmosphereSilicatesGeochemistryMarsWaterMineralogyWindMars Exploration Programengineering.materialFerric CompoundsDiagenesisImpact craterConcretionengineeringSiliciclasticSedimentary rockComposition of MarsSpacecraftEvolution PlanetaryGeologyScience
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The Spirit Rover's Athena science investigation at Gusev Crater, Mars.

2004

The Mars Exploration Rover Spirit and its Athena science payload have been used to investigate a landing site in Gusev crater. Gusev is hypothesized to be the site of a former lake, but no clear evidence for lacustrine sedimentation has been found to date. Instead, the dominant lithology is basalt, and the dominant geologic processes are impact events and eolian transport. Many rocks exhibit coatings and other characteristics that may be evidence for minor aqueous alteration. Any lacustrine sediments that may exist at this location within Gusev apparently have been buried by lavas that have undergone subsequent impact disruption.

BasaltgeographyGeologic SedimentsGeological PhenomenaMineralsMultidisciplinarygeography.geographical_feature_categoryExtraterrestrial EnvironmentLithologyAtmosphereMarsWaterGeologyMars Exploration ProgramWindGeologic SedimentsAstrobiologyVolcanic rockIgneous rockMagneticsImpact craterComposition of MarsGeologyScience (New York, N.Y.)
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Athena Mars rover science investigation

2003

[1] Each Mars Exploration Rover carries an integrated suite of scientific instruments and tools called the Athena science payload. The primary objective of the Athena science investigation is to explore two sites on the Martian surface where water may once have been present, and to assess past environmental conditions at those sites and their suitability for life. The remote sensing portion of the payload uses a mast called the Pancam Mast Assembly (PMA) that provides pointing for two instruments: the Panoramic Camera (Pancam), and the Miniature Thermal Emission Spectrometer (Mini-TES). Pancam provides high-resolution, color, stereo imaging, while Mini-TES provides spectral cubes at mid-inf…

MartianScientific instrumentMeridiani PlanumAtmospheric ScienceThermal Emission SpectrometerEcologySpectrometerPaleontologySoil ScienceForestryAquatic ScienceOceanographyMars roverGeophysicsStereo imagingSpace and Planetary ScienceGeochemistry and PetrologyMartian surfaceEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyRemote sensingJournal of Geophysical Research: Planets
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Magnetic Properties Experiments on the Mars Exploration Rover Spirit at Gusev Crater

2004

The magnetic properties experiments are designed to help identify the magnetic minerals in the dust and rocks on Mars—and to determine whether liquid water was involved in the formation and alteration of these magnetic minerals. Almost all of the dust particles suspended in the martian atmosphere must contain ferrimagnetic minerals (such as maghemite or magnetite) in an amount of ∼2% by weight. The most magnetic fraction of the dust appears darker than the average dust. Magnetite was detected in the first two rocks ground by Spirit.

Geologic SedimentsMineralsMultidisciplinaryExtraterrestrial EnvironmentMagnetic mineralsAtmosphereIronSpinelMarsWaterMaghemiteMineralogyOxidesMars Exploration ProgramAtmosphere of Marsengineering.materialFerrosoferric OxideMagneticschemistry.chemical_compoundImpact craterchemistryFerrimagnetismengineeringGeologyMagnetite
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Overview of the Opportunity Mars Exploration Rover Mission to Meridiani Planum: Eagle Crater to Purgatory Ripple

2006

The Mars Exploration Rover Opportunity touched down at Meridiani Planum in January 2004 and since then has been conducting observations with the Athena science payload. The rover has traversed more than 5 km, carrying out the first outcrop-scale investigation of sedimentary rocks on Mars. The rocks of Meridiani Planum are sandstones formed by eolian and aqueous reworking of sand grains that are composed of mixed fine-grained siliciclastics and sulfates. The siliciclastic fraction was produced by chemical alteration of a precursor basalt. The sulfates are dominantly Mg-sulfates and also include Ca-sulfates and jarosite. The stratigraphic section observed to date is dominated by eolian bedfor…

Meridiani PlanumAtmospheric ScienceEarth scienceGeochemistrySoil ScienceAquatic Scienceengineering.materialOceanographyGeochemistry and PetrologyConcretionStratigraphic sectionEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyBedrockPaleontologyForestryMars Exploration ProgramGeophysicsSpace and Planetary ScienceengineeringAeolian processesSiliciclasticSedimentary rockGeologyJournal of Geophysical Research: Planets
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Indication of drier periods on Mars from the chemistry and mineralogy of atmospheric dust

2005

The cover shows part of the Larry's Lookout panorama, seen from the Mars Exploration Rover (MER) Spirit during its drive up Husband Hill: the summit is about 200 metres from the rover. Six papers this week report in detail on the MER mission. An Analysis compares predictions used to select a landing site with the conditions actually encountered. This ‘ground truth’ will be invaluable for interpreting future remote-sensing data. Surface chemistry suggests that the upper layer of soil may contain 1% meteoritic material. MER provides a unique glimpse of solar transits of the moons Phobos and Deimos. Rover Opportunity examined wind-related processes, and spectroscopy indicates a dry origin for …

Moons of MarsBasaltMultidisciplinaryImpact craterDust stormMineralogyContext (language use)Mars Exploration ProgramAtmosphere of MarsExploration of MarsAstrobiologyNature
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Nickel on Mars: Constraints on meteoritic material at the surface

2006

[1] Impact craters and the discovery of meteorites on Mars indicate clearly that there is meteoritic material at the Martian surface. The Alpha Particle X-ray Spectrometers (APXS) on board the Mars Exploration Rovers measure the elemental chemistry of Martian samples, enabling an assessment of the magnitude of the meteoritic contribution. Nickel, an element that is greatly enhanced in meteoritic material relative to samples of the Martian crust, is directly detected by the APXS and is observed to be geochemically mobile at the Martian surface. Correlations between nickel and other measured elements are used to constrain the quantity of meteoritic material present in Martian soil and sedimen…

MartianAtmospheric ScienceEcologyPaleontologySoil ScienceForestryMartian soilMars Exploration ProgramAquatic ScienceAlpha particle X-ray spectrometerOceanographyExploration of MarsAstrobiologyGeophysicsImpact craterMeteoriteSpace and Planetary ScienceGeochemistry and PetrologyMartian surfaceEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Planets
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Rational and design of the European randomized Optical Coherence Tomography Optimized Bifurcation Event Reduction Trial (OCTOBER)

2018

Background Percutaneous coronary intervention in complex bifurcation lesions is prone to suboptimal implantation results and is associated with increased risk of subsequent clinical events. Angiographic ambiguity is high during bifurcation stenting, but it is unknown if procedural guidance by intravascular optical coherence tomography (OCT) improves clinical outcome. Methods and design OCTOBER is a randomized, investigator-initiated, multicenter trial aimed to show superiority of OCT-guided stent implantation compared to standard angiographic-guided implantation in bifurcation lesions. The primary outcome measure is a 2-year composite end point of cardiac death, target lesion myocardial inf…

Target lesionMalemedicine.medical_specialtyBiolääketieteet - Biomedicinemedicine.medical_treatment030204 cardiovascular system & hematologyCoronary AngiographyLesion03 medical and health sciences0302 clinical medicinePercutaneous Coronary InterventionMulticenter trialmedicineHumans030212 general & internal medicineMyocardial infarctionTomographyAgedUnstable anginabusiness.industrySisätaudit - Internal medicineCoronary StenosisPercutaneous coronary interventionStentDrug-Eluting StentsMiddle Agedmedicine.diseaseCoronary VesselsStenosisTreatment OutcomeOptical CoherenceSettore MED/11 - MALATTIE DELL'APPARATO CARDIOVASCOLAREFemaleRadiologymedicine.symptomCardiology and Cardiovascular MedicinebusinessTomography Optical CoherenceAmerican Heart Journal
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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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An integrated view of the chemistry and mineralogy of martian soils

2005

The mineralogical and elemental compositions of the martian soil are indicators of chemical and physical weathering processes. Using data from the Mars Exploration Rovers, we show that bright dust deposits on opposite sides of the planet are part of a global unit and not dominated by the composition of local rocks. Dark soil deposits at both sites have similar basaltic mineralogies, and could reflect either a global component or the general similarity in the compositions of the rocks from which they were derived. Increased levels of bromine are consistent with mobilization of soluble salts by thin films of liquid water, but the presence of olivine in analysed soil samples indicates that the…

Meridiani PlanumMultidisciplinaryOlivineSoil testMars Exploration RoverMineralogyWeatheringMartian soilengineering.materialmartian soilRocknestSoil waterengineeringComposition of Mars
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Spirit Mars Rover Mission to the Columbia Hills, Gusev Crater: Mission overview and selected results from the Cumberland Ridge to Home Plate

2008

This paper summarizes the Spirit rover operations in the Columbia Hills of Gusev Crater from sols 513 to 1476 and provides an overview of selected findings that focus on synergistic use of the Athena Payload and comparisons to orbital data. Results include discovery of outcrops (Voltaire) on Husband Hill that are interpreted to be altered impact melt deposits that incorporated local materials during emplacement. Evidence for extensive volcanic activity and aqueous alteration in the Inner Basin is also detailed, including discovery and characterization of accretionary lapilli and formation of sulfate, silica, and hematite-rich deposits. Use of Spirit's data to understand the range of spectra…

Atmospheric Sciencegeographygeography.geographical_feature_categoryEcologyWater on MarsPaleontologySoil ScienceForestryMars Exploration ProgramAquatic ScienceOceanographyExploration of MarsCRISMAstrobiologyMars roverGeophysicsVolcanoImpact craterSpace and Planetary ScienceGeochemistry and PetrologyRidgeEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Overview of the magnetic properties experiments on the Mars Explorations Rovers

2009

[1] The Mars Exploration Rovers have accumulated airborne dust on different types of permanent magnets. Images of these magnets document the dynamics of dust capture and removal over time. The strongly magnetic subset of airborne dust appears dark brown to black in Panoramic Camera (Pancam) images, while the weakly magnetic one is bright red. Images returned by the Microscopic Imager reveal the formation of magnetic chains diagnostic of magnetite-rich grains with substantial magnetization (>8 Am2 kg−1). On the basis of Mossbauer spectra the dust contains magnetite, olivine, pyroxene, and nanophase oxides in varying proportions, depending on wind regime and landing site. The dust contains a …

Atmospheric ScienceSoil ScienceMineralogyPyroxeneAquatic Scienceengineering.materialOceanographychemistry.chemical_compoundMagnetizationGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and TechnologyMagnetiteBasaltOlivineEcologySpinelPaleontologyForestryMars Exploration Programequipment and suppliesSilicateGeophysicschemistrySpace and Planetary ScienceengineeringGeology
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