Search results for "TCR"

showing 10 items of 157 documents

Mineralogy and chemistry of cobbles at Meridiani Planum, Mars, investigated by the Mars Exploration Rover Opportunity

2010

Numerous loose rocks with dimensions of a few centimeters to tens of centimeters and with no obvious physical relationship to outcrop rocks have been observed along the traverse of the Mars Exploration Rover Opportunity. To date, about a dozen of these rocks have been analyzed with Opportunity’s contact instruments, providing information about elemental chemistry (Alpha Particle X‐ray Spectrometer), iron mineralogy and oxidation states (Mossbauer Spectrometer) and texture (Microscopic Imager). These "cobbles" appear to be impact related, and three distinct groups can be identified on the basis of chemistry and mineralogy. The first group comprises bright fragments of the sulfate‐rich bedroc…

Meridiani PlanumBasaltAtmospheric Sciencegeographygeography.geographical_feature_categoryEcologyOutcropBedrockPaleontologySoil ScienceMineralogyForestryMars Exploration ProgramAquatic ScienceOceanographyMesosideriteGeophysicsMeteoriteSpace and Planetary ScienceGeochemistry and PetrologyGroup (stratigraphy)Earth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Two Years at Meridiani Planum: Results from the Opportunity Rover

2006

The Mars Exploration Rover Opportunity has spent more than 2 years exploring Meridiani Planum, traveling ∼8 kilometers and detecting features that reveal ancient environmental conditions. These include well-developed festoon (trough) cross-lamination formed in flowing liquid water, strata with smaller and more abundant hematite-rich concretions than those seen previously, possible relict “hopper crystals” that might reflect the formation of halite, thick weathering rinds on rock surfaces, resistant fracture fills, and networks of polygonal fractures likely caused by dehydration of sulfate salts. Chemical variations with depth show that the siliciclastic fraction of outcrop rock has undergon…

Meridiani PlanumGeologic SedimentsExtraterrestrial EnvironmentOutcropGeochemistryMarsMineralogyWeatheringengineering.materialFerric CompoundsTimeConcretionSpacecraftMineralsMultidisciplinarySulfatesSilicatesWaterHematitevisual_artengineeringvisual_art.visual_art_mediumHaliteSedimentary rockSiliciclasticAcidsGeologyScience
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Jarosite and hematite at Meridiani Planum from Opportunity's Mossbauer Spectrometer.

2004

Mössbauer spectra measured by the Opportunity rover revealed four mineralogical components in Meridiani Planum at Eagle crater: jarosite- and hematite-rich outcrop, hematite-rich soil, olivine-bearing basaltic soil, and a pyroxene-bearing basaltic rock (Bounce rock). Spherules, interpreted to be concretions, are hematite-rich and dispersed throughout the outcrop. Hematitic soils both within and outside Eagle crater are dominated by spherules and their fragments. Olivine-bearing basaltic soil is present throughout the region. Bounce rock is probably an impact erratic. Because jarosite is a hydroxide sulfate mineral, its presence at Meridiani Planum is mineralogical evidence for aqueous proc…

Meridiani PlanumGeologic SedimentsExtraterrestrial EnvironmentOutcropMineralogyMagnesium CompoundsMarsengineering.materialFerric CompoundsSpectroscopy MossbauerImpact craterConcretionJarositeComposition of MarsSpacecraftMineralsMultidisciplinaryMineralSulfatesSilicatesWaterHematitevisual_artvisual_art.visual_art_mediumengineeringGeologyIron CompoundsScience (New York, N.Y.)
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Chemistry and mineralogy of outcrops at Meridiani Planum

2005

Analyses of outcrops created by the impact craters Endurance, Fram and Eagle reveal the broad lateral continuity of chemical sediments at the Meridiani Planum exploration site on Mars. Approximately ten mineralogical components are implied in these salt-rich silicic sediments, from measurements by instruments on the Opportunity rover. Compositional trends in an apparently intact vertical stratigraphic sequence at the Karatepe West ingress point at Endurance crater are consistent with non-uniform deposition or with subsequent migration of mobile salt components, dominated by sulfates of magnesium. Striking variations in Cl and enrichments of Br, combined with diversity in sulfate species, pr…

Meridiani PlanumOutcropGeochemistrySilicicMineralogychemistry.chemical_compoundIgneous rockGeophysicschemistryImpact craterSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Sedimentary rockSulfateMaficGeologyEarth and Planetary Science Letters
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Soils of Eagle crater and Meridiani Planum at the Opportunity Rover landing site.

2004

The soils at the Opportunity site are fine-grained basaltic sands mixed with dust and sulfate-rich outcrop debris. Hematite is concentrated in spherules eroded from the strata. Ongoing saltation exhumes the spherules and their fragments, concentrating them at the surface. Spherules emerge from soils coated, perhaps from subsurface cementation, by salts. Two types of vesicular clasts may represent basaltic sand sources. Eolian ripples, armored by well-sorted hematite-rich grains, pervade Meridiani Planum. The thickness of the soil on the plain is estimated to be about a meter. The flatness and thin cover suggest that the plain may represent the original sedimentary surface.

Meridiani PlanumRover Landing SiteGeologic SedimentsMineralsMultidisciplinaryExtraterrestrial EnvironmentOutcropSilicatesSpectrum AnalysisGeochemistryMineralogyMarsWaterHematiteFerric CompoundsImpact craterClastic rockvisual_artvisual_art.visual_art_mediumAeolian processesSedimentary rockMeridiani PlanumSpacecraftGraded beddingGeologyScience (New York, N.Y.)
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Degree of terrestrial activity of the elusive sun-tailed monkey (Cercopithecus solatus) in Gabon: Comparative study of behavior and postcranial morph…

2015

We carried out a multidisciplinary study linking behavioral and morphological data from a little-known guenon species, Cercopithecus solatus, endemic to Gabon. Over a period of 9 months, we documented the pattern of stratum use associated with postural and locomotor behavior by direct observation (650 hrs) of a semi-free-ranging breeding colony. We also conducted a morphometric analysis of the humerus and limb proportions of 90 adult specimens from 16 guenon species, including C. solatus. Field observations indicated that C. solatus monkeys spent a third of their time on the ground, similar to semi-terrestrial guenon species. We detected two patterns of stratum use: at ground level, and in …

MorphometricsbiologyEcologyCercopithecus solatusDirect observationPostcraniaZoologybiology.organism_classificationGuenonGround levelDry seasonAnimal Science and ZoologyAdaptationEcology Evolution Behavior and SystematicsAmerican Journal of Primatology
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Spanish Stock Returns: Rational or Weather-Influenced?

2002

Psychological studies support the existence of an influence of weather on mood. It could affect the behaviour of market traders, as suggested by some authors, and this should be reflected by the stock returns. This paper investigates the possible relation between weather and market index returns in the context of the Spanish market, in order to test the above hypothesis. In 1989, this market changed its open outcry trading system into a computerised and decentralised trading system. Therefore, it is possible to check the influence of weather variables (sunshine hours and humidity levels) on index returns in an open outcry trading system, and to compare it with a screen traded environment. T…

Open outcryFinancial economicsSunshine durationEconomicsAlgorithmic tradingcomputer.software_genreCONTESTEmpirical evidencecomputerStock market indexStock (geology)SSRN Electronic Journal
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Predicting the landslides triggered by the 2009 96E/Ida tropical storms in the Ilopango caldera area (El Salvador, CA): optimizing MARS-based model b…

2019

The main topic of this research was to evaluate the effect in the performance of stochastic landslide susceptibility models, produced by differences between the triggering events of the calibration and validation datasets. In the Caldera Ilopango area (El Salvador), MARS (multivariate adaptive regression splines)-based susceptibility modeling was applied using a set of physical–environmental predictors and two remotely recognized landslide inventories: one dated at 2003 (1503 landslides), which was the result of a normal rainfall season, and one which was produced by the combined effect of the Ida hurricane and the 96E tropical depression in 2009 (2237 landslides). Both the event inventorie…

OutcropCalibration (statistics)Settore GEO/04 - Geografia Fisica E Geomorfologia0208 environmental biotechnologySoil SciencePyroclastic rock02 engineering and technology010501 environmental sciences01 natural sciencesEnvironmental ChemistryCalderaTemporal validation0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyIda hurricaneGlobal and Planetary ChangeMultivariate adaptive regression splinesMARSGeologyLandslideCaldera Ilopango (El Salvador)Mars Exploration ProgramLandslide susceptibilityPollution020801 environmental engineeringPhysical geographyTropical cycloneGeology
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Ladinian carbonates of the Cabo Cope Unit (Betic Cordillera, SE Spain): a tethys-maláguide palaeogeographic gateway.

2003

7 pages, 4 figures.

OutcropCarbonate platformDaonellaStratigraphyMaláguide ComplexSephardiellaPaleontologychemistry.chemical_compoundDaonellaPosidoniaSedimentologyTethysbiologyTriassic (Ladinian)PaleontologyGeologyLadinianbiology.organism_classificationBetic BasinchemistrySpainClastic rockAlpine Faunal ProvinceCarbonate PlatformCarbonate rockCarbonatePalaeogeographyGeologySephardic Faunal Province
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A foraminiferal assemblage as a bioevent marker of the main Ladinian transgressive stage in the Betic Cordillera, southern Spain

2005

Abstract The Betic Cordillera comprises the mountain range in the southern Iberian Peninsula that extends from Cadiz to Alicante, which displays typical features of alpine cordilleras. The Betic Cordillera includes two large geological tectonic domains, namely an External Zone, and an Internal Zone. The External Zone is essentially composed of epicontinental Triassic rocks that consist of the Buntsandstein, Muschelkalk and Keuper facies. The Buntsandstein facies rarely occur in outcrops, whereas the Keuper stratigraphic successions are truncated. The Muschelkalk facies frequently displays complete successions that are very useful for interpreting the Ladinian stage palaeogeography. The Musc…

OutcropPaleontologyKeuperLadinianOceanographyPaleontologyStage (stratigraphy)FaciesMarlTransgressiveEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesMarine transgressionPalaeogeography, Palaeoclimatology, Palaeoecology
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