#LPSC2023
#LPSC2023
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Poster Session: Volcanism Across the Solar System
Tuesday, March 14, 2023, 6:30 PM
Town Center Exhibit Hall
Balme M. R.*
Grindrod P. M.
Jay A. E.
Linear Ridges in Arabia Terra, Mars: An Ancient Giant Radiating Dyke Swarm?
[#2226]
The distribution and morphology of ~10,000 highly linear ridges in Arabia Terra, Mars, are presented. The ridges are interpreted to be a radiating dyke swarm.
The distribution and morphology of ~10,000 highly linear ridges in Arabia Terra, Mars, are presented. The ridges are interpreted to be a radiating dyke swarm.
Mohr K. M.*
Williams D. A.
Garry W. B.
Revised Geologic Mapping of Ascraeus Mons, Mars
[#2601]
Ascraeus Mons shield, built and buried by lava, modified by time.
Ascraeus Mons shield, built and buried by lava, modified by time.
Peters S. I.*
A Survey of Volcanically Emplaced Rilles on Mars
[#1713]
A global survey of volcanically emplaced rilles has been undertaken on Mars in order to understand and constrain its volcanic evolution.
A global survey of volcanically emplaced rilles has been undertaken on Mars in order to understand and constrain its volcanic evolution.
Plescia J. B.*
Late Stage Lunar Lava Flows and Cinder Cones
[#2741]
Low-volume wide-distribution volcanism indicates many sources survived late in time and is inconsistent with ideas of late high-volume/effusion rate volcanism.
Low-volume wide-distribution volcanism indicates many sources survived late in time and is inconsistent with ideas of late high-volume/effusion rate volcanism.
Gansler K.*
Montési L.
Lekić V.
Gravity Signature of Valles Schröteri and the Possibility of Detecting Lava Tubes Associated with Sinuous Rilles
[#1328]
Free air gravity anomalies near Valles Schröteri give possible indication of a large subsurface void along a portion of the sinuous rille.
Free air gravity anomalies near Valles Schröteri give possible indication of a large subsurface void along a portion of the sinuous rille.
Adeloye A. O.*
Goldstein D. B.
Trafton L. M.
Varghese P. L.
Mahieux A.
DSMC Modeling of Tvashtar Eruption: Matching Simulation Results of Two-Phase Flow with New Horizons LORRI and MVIC Observations
[#2489]
We present an approach to analyze New Horizons images of Io’s Tvashtar eruption to explain unexpected increase in plume brightness during flyby period in 2007.
We present an approach to analyze New Horizons images of Io’s Tvashtar eruption to explain unexpected increase in plume brightness during flyby period in 2007.
Vaci Z.*
Gillis-Davis J. J.
Ogliore R. C.
Koefoed P.
Experimental Analog for High-Speed Particle Capture from Io Volcanic Plume
[#1370]
Bulk chemical digestion and ICP-MS analysis of analog materials implanted at high energy onto novel substrates.
Bulk chemical digestion and ICP-MS analysis of analog materials implanted at high energy onto novel substrates.
Nolan J. A.*
Graettinger A. H.
Small-Volume Igneous Landforms and Edifices Statistics (SMILES): A Database of Dimensionless Parameters of Terrestrial Analogs for Remote Sensing Volcanic Landforms
[#2927]
A catalog of dimensionless parameters that enable remote sensing of terrestrial and non-terrestrial volcanic landforms.
A catalog of dimensionless parameters that enable remote sensing of terrestrial and non-terrestrial volcanic landforms.
Munoz-Rojas B.*
Flahaut J.
Larrea P.
Ford M.
France L.
et al.
Topographic Data, Petrography, and Sample Geochemistry as Proxies to Constrain Lava Flow Rheology: "The Case of the Altiplano-Puna Volcanic Complex Mars Analogue Site"
[#1515]
Remote sensing, petrography, and petrology analyses of single terrestrial lava flows from the Altiplano-Puna volcanic complex, northern Chile.
Remote sensing, petrography, and petrology analyses of single terrestrial lava flows from the Altiplano-Puna volcanic complex, northern Chile.
Sehlke A.*
Whittington A. G.
New Model to Calculate Lava Viscosity During Disequilibrium Crystallization for a Wide Range in Cooling and Strain Rates
[#2677]
Developed a new model to calculate the viscosity of crystallizing lava as a function of cooling rate. Further work to include strain-rate dependence underway.
Developed a new model to calculate the viscosity of crystallizing lava as a function of cooling rate. Further work to include strain-rate dependence underway.
Wang J.
Schmerr N.
Bell E.*
McCall N.
Wike L.
et al.
Near-Surface Results of Active Seismic Transects of the Rim and Crater of the Kilbourne Hole, NM Maar Volcanic Crater
[#2926]
Active seismic refraction and reflection study to examine the rim and crater structure of the Kilbourne Hole maar volcano as an analog to martian maar craters.
Active seismic refraction and reflection study to examine the rim and crater structure of the Kilbourne Hole maar volcano as an analog to martian maar craters.
Hottendorf K. H.*
Sakimoto S. E. H.
Paredes M. S.
Gregg T. K. P.
Rock Corral Butte, Eastern Snake River Plain, Idaho: A Low Shield Volcano Emplaced by Pressurized, Insulated Flow
[#2644]
Encrusted flow lobes / Advances, then stops, then goes / Ruptures at their toes.
Encrusted flow lobes / Advances, then stops, then goes / Ruptures at their toes.
Wróblewski F. B.*
Rader E. L.
Detecting Glass on the Krafla Lava Flow Field, Iceland
[#1802]
Dark basalts are flat. / You know what’s even flatter? / The spectra of glass.
Dark basalts are flat. / You know what’s even flatter? / The spectra of glass.
Burton Z. F. M.*
Rader E. L.
Chemical Variability Between Lava Vents and Lava Surfaces — Margins: Black Crater and Ross Flow, Lava Beds National Monument, California, USA
[#1211]
We analyze Californian basalt flows / Intraflow chemical variability, XRF shows / Notable for volcanic bodies among the stars / Like Mercury, the Moon, and Mars.
We analyze Californian basalt flows / Intraflow chemical variability, XRF shows / Notable for volcanic bodies among the stars / Like Mercury, the Moon, and Mars.
Klemme S.*
Renggli C. J.
Experimental Constraints on Stable Isotope Fractionation Due to Evaporation from Silicate Melts
[#1537]
Experimental results on elemental and isotope fractionation of moderately volatile elements.
Experimental results on elemental and isotope fractionation of moderately volatile elements.
Vannier H.*
Horgan B.
VNIR Spectral Properties of Felsic Rocks: Implications for Mars Detections
[#2831]
We interpret VNIR spectra of felsic rocks, and detect plagioclase at lower wt% than previously recognized. We discuss in the context of Mars plag detections.
We interpret VNIR spectra of felsic rocks, and detect plagioclase at lower wt% than previously recognized. We discuss in the context of Mars plag detections.
Barthez M.*
Flahaut J.
Guitreau M.
Ito G.
Pik R.
Petrological, Geochemical and Spectral Laboratory Studies of Terrestrial Feldspathic Rocks: Understanding Plagioclase Signatures in the VNIR Domain as an Analog to Mars
[#1511]
Elaboration of a database containing VNIR reflectance spectra acquired on characterized macroscopic samples of various terrestrial feldspar-bearing rocks.
Elaboration of a database containing VNIR reflectance spectra acquired on characterized macroscopic samples of various terrestrial feldspar-bearing rocks.
Varatharajan I.*
Sklute E.
Glotch T. D.
Dyar M. D.
A Genetic Algorithm Approach for Obtaining Wavelength Dependent Mid-Infrared Optical Constants (5-25 µm) of Silicate Glasses
[#1665]
The study presents genetic algorithm approach for numerical modeling of wavelength dependent MIR optical constants of silicate glasses of varying SiO2 content.
The study presents genetic algorithm approach for numerical modeling of wavelength dependent MIR optical constants of silicate glasses of varying SiO2 content.
Zhang P. F.
Jin Z. L.*
Wiedenbeck M.
Glynn S.
Couffignal F.
The Formation of Early Andesitic Magmas Triggered by Hybrid Accretion
[#2116]
Our mineralogy and isotopic studies on the minerals in the meteorite EC002 revealed a distinct evolutional history of its parent body.
Our mineralogy and isotopic studies on the minerals in the meteorite EC002 revealed a distinct evolutional history of its parent body.
Huang D.*
Murakami M.
Brodholt J.
McCammon C.
Petitgirard S.
Pressure-Induced Smooth Structural Evolution in a Terrestrial Magma Ocean
[#2248]
In less polymerized silicate melt, pressure-induced structural transition is more protracted than previously proposed.
In less polymerized silicate melt, pressure-induced structural transition is more protracted than previously proposed.
*presenter