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Silicic volcanism on Mars evidenced by tridymite in high-SiO2 sedimentary rock at Gale craterThe first X-ray diffraction measurements on Mars.The origin and implications of clay minerals from Yellowknife Bay, Gale crater, Mars.An integrated view of the chemistry and mineralogy of martian soils.Clay mineral diversity and abundance in sedimentary rocks of Gale crater, Mars.Mars Science Laboratory Mission and Science InvestigationBackground levels of methane in Mars’ atmosphere show strong seasonal variationsCharacterization and Calibration of the CheMin Mineralogical Instrument on Mars Science LaboratoryBounce Rock-A shergottite-like basalt encountered at Meridiani Planum, MarsAtmospheric Electron Induced X-Ray Spectrometer (AEXS) DevelopmentLong-term volumetric eruption rates and magma budgetsMars Exploration Rover Science Results: This Past Year's HighlightsSelecting landing sites for the 2003 Mars Exploration RoversMars Exploration Rover missionInfluence of volatile loss on thickness and density profiles of active basaltic flow lobesCharacteristics of the Pathfinder APXS sites: Implications for the composition of Martian rocks and soilsSoil-like deposits observed by Sojourner, the Pathfinder roverEruption constraints on tube-fed planetary lava flowsDesign of a miniature solid state NIR spectrometerThe infrared spectrum of H2S from 1 to 5 μmInfluence of crystallization and entrainment of cooler material on the emplacement of basaltic aa lava flowsFourier-transform spectrum of H 2 S in 2000 - 9000 cm-1A novel miniature spectrometer using an integrated acousto‐optic tunable filterCrystallization history of the 1984 Mauna Loa lava flowMid-infrared spectroscopy of Pahala ash palagonite and implications for remote sensing studies of MarsAnalysis of active volcanoes from the earth observing systemA method for estimating eruption rates of planetary lava flowsA model for lava flows with two thermal componentsThermal infrared spectral character of Hawaiian basaltic glassesPyroclastic flows and lavas of the Mogan and Fataga formations, Tejeda Volcano, Gran Canaria, Canary Islands: mineral chemistry, intensive parameters, and magma chamber evolutionPhase relations to 3 kbar in the systems edenite + H2O and edenite + excess quartz + H2ORates of magma emplacement and volcanic outputCILIMUS: A NEW CHONDRITE FALLTHE TAMBAKWATU CHONDRITEEruption volume, periodicity, and caldera area: Relationships and inferences on development of compositional zonation in silicic magma chambers
P50
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P50
description
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
Joy Crisp
@ast
Joy Crisp
@en
Joy Crisp
@es
Joy Crisp
@nl
type
label
Joy Crisp
@ast
Joy Crisp
@en
Joy Crisp
@es
Joy Crisp
@nl
altLabel
Joy A. Crisp
@en
Joy Anne Crisp
@en
Joy Miller
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prefLabel
Joy Crisp
@ast
Joy Crisp
@en
Joy Crisp
@es
Joy Crisp
@nl
P106
P31
P496
0000-0002-3202-4416