Washington University in Saint Louis, Department of Earth and Planetary Science

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    I[Washington University in Saint Louis, Department of Earth and Planetary Science]
    PI["Parent Institutions (1)"]
    CI["Child Institutions (0)"]
    AW["Affiliated Works (626)"]
    CA["Linked Collaborating Authors (10)"]
    I== skos:broader ==>PI
    CI== skos:broader ==>I
    AW== affil ==>I
    AW== author ==>CA
    click PI "#parent-institutions"
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ADS ID [?]

A01256

Abbreviation [?]

Dep Ear Plan Sci

Parent Institutions [?]

• Washington University in Saint Louis, Missouri

Child Institutions [?]

Affiliated Works

sorted by decreasing year, and then by display-name

• A Simulated Annealing Procedure for the Joint Inversion of Spectroscopic and Compositional Data.
• A Truncated Virial Equation of State for Components of Hydrothermal/Magmatic Fluids
• Constraints on the Character of Plate Tectonics From the Study of Diffuse Plate Boundaries
• Development and Field Testing of a Rover-Deployable Ground Penetrating Radar
• Dynamic controls on the initiation of extension in continental and oceanic crust
• Folding in a Cooling Crust with Elasto-visco-plastic Rheology: An Example from Venus
• Lithium Budget and Isotopic Characterization of Materials Entering the Izu-Mariana Subduction Zone
• Lithologic Mapping in the Southern Soda Mountains, Mojave Desert, Using ASTER Data
• Mapping Lithologic Units Exposed on the Summit of Mauna Kea Using AVIRIS Hyperspectral Reflectance Data
• Mapping Sn Velocities
• Mapping the base of the mantle with global digital Sdiff waves.
• New Radar Observations of Terra Meridiani, Mars.
• New constraints on element transfer rates beneath the Tonga-Kermadec arc from combined U-Th-Ra, U-Pa and Be isotope data
• Noble gas Records of Early Evolution of the Earth
• Numerical Models of Decompression Melting at Volcanic Arcs
• Outer Rise Seismicity at the Tonga Trench Recorded by Ocean Bottom Seismographs
• Oxygen Isotope Record of Hydrothermal Flow along Normal Faults, Comstock Lode, NV.
• Seismic Body Wave Constraint on Mechanisms of Intermediate-Depth Earthquakes
• Seismicity and Tectonics of the South Shetland Islands Region From a Combined Land-Sea Seismograph Deployment
• Terrestrial Chemical Alteration of Hot Desert Meteorites
• The Influence of the Temperature-Dependence of Phonon Lifetimes in Lattice Thermal Conductivity on Mantle Convection
• The Martian Surface at Human Scales: Using MOLA Data to Improve Earth-based Radar Scattering Model Retrievals
• Thermal Conductivity of Garnets and the Middle Mantle
• Thermal Inertia, Albedo and MOLA-Derived Roughness for Terrains in the Terra Meridiani Area, Mars
• Understanding the Global Geological History of Mars: The Contributions of Mars Global Surveyor
• Volcanism, Clouds, and the Climate of Early Mars
• <SUP>10</SUP>Be Systematics of Incoming Sediments and Arc Lavas at the Izu and Mariana Convergent Margin
• Archiving Data From the 2003 Mars Exploration Rover Mission
• Crustal and Upper Mantle Structure of Southernmost South America Inferred from Regional Waveform Inversion
• Development of a Laser Raman Spectrometer for In Situ Measurements in the Deep Ocean
• Earth's Heat Flux and Links to Chemistry
• Effects of Early Water-Rock Chemical Interactions on Interior Structures, Physical Properties, and Heat Balances of Galilean Satellites
• Energetics of Nitrogen Biogeochemistry in Hot Spring Habitats
• Field Observations Using the FIDO Infrared Point Spectrometer: Mineralogical Interpretation and Implications for In Situ Investigations on Mars
• Hematite and Etched Terrain Distribution in Terra Meridiani, Mars
• Hydroxyl Impurities Enhance Radiative Transfer in the Upper Mantle
• Hyperspectral Mapping and Identification of Lava Flows, Ash Deposits, and Solfataras in the Ka'u Desert, Hawai'i
• Ion-irradiation of materials spectrally similar to the non-ice surface of Callisto
• Mantled and Exhumed Terrains in Terra Meridiani, Mars
• Mapping Lithologic Units on Cinder Cones at the Summit of Mauna Kea Using AVIRIS Hyperspectral Reflectance Data
• Mars Exploration Rovers as Virtual Instruments for Determination of Terrain Roughness and Physical Properties
• Mineralogical Ground Truth for AVIRIS Hyperspectral Observations of Cinder Cones on the Summit of Mauna Kea Volcano
• Optical Constants of Planetary Analogs Using KBr Pellet Transmission
• Origin and Composition of the Rock+Metal Interiors of the Galilean Satellites
• P and S-wave Tomography of the Tonga Arc and Lau Back-Arc Basin
• Radar Scattering Properties of Terra Meridiani, Mars
• Remote triggering and aftershocks of deep earthquakes
• Sedimentation History in Western Pacific Affects Along-strike Variations in Izu-Bonin-Mariana-Honshu Arc Volcanics
• Selection and Evaluation of Landing Sites for the Mars Exploration Rovers
• Short-wavelength Contractional Structures in Venusian Fold Belts: Additional Constraints From New Models
• Simulated Mars Rover Mission to Hydrothermal Vents, Ka'u Desert, Hawai'i
• Simulating a MER Landing Site Remote Sensing Data Set for the 2002 FIDO Field Test
• Source Characteristics of the August 19, 2002 Tongan Deep Earthquakes
• The Seismic Structure of Subduction Zones: Implications for Subduction Dynamics and Volatile Recycling
• Thermal Stresses and Mountain Building on Io.
• Why Microbial Ecology and Ecogenomics Needs Geochemistry: An Illustrated Example
• Anatahan Eruption of May, 2003: Integrated Response of the MARGINS Community
• Attenuation at the base of the mantle: Global mapping using core-reflected and core-diffracted waves
• Callisto and Titan: What Lies Beneath?
• Constraints on the Mechanism and Timing of Sediment Recycling Beneath the Tonga-Kermadec arc From Be isotopes
• Could Low Thermal Diffusivity Provide Runaway Melting in The Upper Mantle?
• Crustal Structure and Mantle Anisotropy from Florida to Edmonton
• Do Lunar Soils Tell us When the Geomagnetic Field First Appeared?
• First Expeditionary Deployments of the Deep Ocean Raman In Situ Spectrometer
• Global Lower Mantle Velocity, Attenuation, and Anisotropy from Differential ScS-S Analysis
• H and C Impurities in Synthetic Majoritic Garnets: Implications for Speciation and Solubility
• High frequency local reflections and conversions from upper mantle discontinuities in the Fiji-Tonga subduction zone
• Implications of Smectite Subduction at the Costa Rican Convergent Margin
• Lateral variations in the structure of the thermal boundary layer at the base of the mantle from the dispersion of core-diffracted waves
• Mapping Hydrothermal Alteration Zones on Mauna Kea Using AVIRIS Data: An Analog for Mars
• Near-antipodal PKPdf observations from the Trans-Antarctic Mountains Seismic Experiment (TAMSEIS): Constraints on inner-core anisotropy from a seismic deployment in Antarctica
• Sediment/Fluid Contributions and Element Transport Deduced from Elemental and Isotopic Data From the Luzon-Bicol arc Systems, Philippines
• Seismic recording of the Anatahan eruption
• Spherical Harmonic Analysis of Mountain and Volcanic Center Distributions on Io
• The Eastern Lau Basin Integrated Studies Site (ISS)
• The Effect of Critical Points in Radiative Thermal Conductivity (With Grain Size and Temperature) on the Transition Zone and Lower Mantle
• The Power of JIMO for Determining Galilean Satellite Internal Structure and Origin
• Theoretical Modeling of Outflow Channels and Chaos Regions on Mars
• Thin Elastic Shell Flexure Models of Possible Ocean Basins on Mars: Preliminary Analysis
• Vp/Vs Tomography of the Central Lau Spreading Center and Tonga Volcanic Arc
• Beryllium Isotope and Combined Be and U-series Isotope Studies of Volcanic Arcs: Implications for Fluid and Melt Transport Through the Mantle Wedge
• Chemistry and Mineralogy of the Regolith at the Gusev Plains
• Cold Compaction of Porous Ice and the Density of Phoebe
• Comprehensive geophysical study of the Transantarctic Mountains
• Computational Infrastructure for Geodynamics (CIG)
• Detailed Structure and Thickness of Upper Mantle Discontinuities in the Tonga Subduction Zone From Regional Broadband Arrays
• Dynamics of Block Rotations in Strike-Slip Fault Zones: A Perspective from Distinct Element Modelling
• Effects of hydrogen impurities on the lattice thermal diffusivity of quartz and quartzites up to 1000\deg C
• Gabbro fracturing and elemental analysis in the Costa Rica margin (ODP Leg 205): Core-log integrated high-resolution study
• Geomorphic and Spectral Mapping of Meridiani Planum Eastern Etched Terrain
• Global Spectral and Compositional Diversity of Mars: A Test of CRISM Global Mapping with Mars Express OMEGA Data
• Implications of Heat Flow in the Triaxial Earth on Layered Convection and Plume Formation
• In Situ Raman Spectra from the SeaCliff Hydrothermal Field (Gorda Ridge)
• Partial Melting of Ordinary Chondrite Under Reducing Conditions
• Petrographic and isotopic (δ <SUP>18</SUP>O, δ <SUP>17</SUP>O, δ <SUP>13</SUP>C, and δ <SUP>14</SUP>C) study of carbonate minerals in a group of paired Antarctic CM2 meteorites.
• Phylogenomic Methods to Guide Paleontological Searches for the Early Cyanobacteria
• Plume-Ridge Interaction on the Cocos Plate (ODP Leg 205, Costa Rica): Implication for Fluid Circulation
• Predictive Microbiology in Hydrothermal Ecosystems
• Radiative Transfer Photometric Analysis of Surface Materials at the Mars Exploration Rover Landing Sites
• Ranking Geochemical Energy Availability in Hydrothermal Ecosystems
• Remote Triggering of Deep Earthquakes - Indication for Criticality of Subducted Slabs
• Scaling of plume formation on Mars
• Seismic activity in the Transantarctic Mountains recorded by the TAMSEIS seismic array.
• Shear Wave Splitting and Seismic Anisotropy in the Mariana Mantle Wedge from a Combined Land-Sea Deployment
• Terrain Roughness from MER Traverse Profiles at Gusev Crater and Meridiani Planum
• The Eastern Lau Basin Integrated Studies Site (ISS): Recent Progress and Future Plans
• The Size-Frequency and Areal Distribution of Rock Clasts at the Spirit Landing Site, Gusev Crater, Mars
• The Threshold Dependencies of Thermal Conductivity and Implications on Mantle Dynamics
• The Viability of Three Simultaneous Melting Mechanisms at Volcanic Arcs
• Thermal Conductivity of Deep Mantle Phases: Grain-size as a Primary Control of Radiative Transfer
• Tilt Recorded by a Portable Broadband Seismograph: The 2003 eruption of Anatahan, Northern Mariana Islands
• Upper Mantle Structure Beneath the Transantarctic Mountains From Body-Wave Tomography and Receiver Functions Using TAMSEIS Data
• VNIR spectral features observed by the Mars Exploration Rover Opportunity in hematite-bearing materials at Meridiani Planum
• Viscoelastic Relaxation of Lunar Basins
• A Broadband Seismological Investigation of the Cameroon Volcanic Line
• A New System of Tectonic Outflow Channels in the Memnonia Region of Mars
• An Overview of Results from the 2003-2004 Mariana Subduction Factory Passive Imaging Experiment
• Convection in large icy satellites with self-consistent grain-size evolution
• Coordinated Analysis of Mars Express OMEGA Hyperspectral Imaging and Mars Exploration Rover Traverse Data for Meridiani Planum
• Deciphering Lower Mantle Structure With the Dispersion of Core-Diffracted Waves
• Demonstrations in Introductory Geophysics
• Earthquake Swarms Detected by the Mariana SUBFAC Seismograph Deployment: Submarine Volcanic Activity and Tectonic Deformation of the Mariana Microplate
• Effects of 3D Velocity and Attenuation in the Tonga-Fiji Subduction Zone
• Examining the Discontinuity Structure of the Base of the Mantle Using Seismic Data From the IRIS PASSCAL FLED Array
• Examining the Mantle Transition Zone Beneath the Transantarctic Mountains From Receiver Functions Using TAMSEIS Data
• First Science Results from MARSIS Subsurface Sounding
• Geomorphic and Spectral Mapping of Meridiani Planum Northern Etched Terrains
• Geophysical Limits to Europan Hydrothermal History
• Global teaching of global seismology
• High-Temperature Thermal Diffusivity Measurements of Silicate Glasses
• Low Temperature Fluid Flow in the Permeable Igneous Complex of the Subducting Cocos Plate, Offshore Costa Rica
• Mars Exploration Program 2007 Phoenix Mission Landing Site Selection
• Metabolic Potential of the Deep Subseafloor at Selected Convergent Margins
• Microbial arsenic oxidation in a shallow marine hydrothermal vent system
• Molecular Studies of Filamentous and Biofilm-Forming Hyperthermophilic Communities in Yellowstone National Park
• North Pacific Transition Zone Thickness From SS-Precursors
• Porous Flow and Diffusion of Water in the Mantle Wedge: Melting and Hydration Patterns
• Recent Results From the Mars Exploration Rover Spirit Mission
• Recent Results from the Mars Exploration Rover Opportunity Mission
• Seismicity of the Shallow Thrust Zone and Celestial and Big Blue Serpentinite Seamounts in the Northern Mariana Arc From Ocean Bottom Seismographs
• Subsurface Structure and the Stress State of the Utopia Basin, Mars
• THEMIS and MOLA Provide 3-D Stratigraphy in the Terra Meridiani Region of Mars
• Unexpected Arsenate/Arsenite Gradients in Pore-Water Profiles From a Shallow-Water Hydrothermal System
• Upper mantle structure beneath the Transantarctic Mountains and East Antarctic Craton from P and S body wave tomography
• A New Look at Factors Affecting Microbial Silicification: Effects of Microbe to Solution Ratio, Al and Fe on Silica Accumulation on B. subtilis Surfaces
• A New Seismic Phase with Ray Parameter = 0: GOOOOOOOOOOOOOAOAOAOAOAOAAAAAAAALLLLLLLLLL!!!
• Archaeal Communities in an Arsenic-Rich Shallow-Sea Hydrothermal System
• Atmospheric Science using CRISM EPF Sequences
• Comparison of Forward Calculated Velocity Structure With Tomographic Images of Subduction Zones
• Constraining Lower Mantle Heterogeneity With Differential Dispersion of Core-Diffracted Waves
• Coordinated Analyses of Orbital and Spirit Rover Data to Characterize the Nature of Surface Materials in Gusev Crater, Mars
• Crust and upper mantle structure beneath the Transantarctic Mountains, East Antarctic Craton and West Antarctic Rift System from the TAMSEIS project
• Detailed Image of the Subducting Plate and Upper mantle Seismic Discontinuities in the Mariana Subduction Zone
• Enhanced Stage Variability on the Lower Missouri River as Benchmarked by Lewis and Clark: Implications for Ecosystem Restoration
• Evidence for a Carbonaceous Chondrite Parent Body With Near-TFL Oxygen Isotopes From Unique Metachondrite Northwest Africa 2788
• Evidence for kinks in structural and thermodynamic properties across the forsterite-fayalite binary from IR spectra
• First Retrieval of Surface Lambert Albedos From Mars Reconnaissance Orbiter CRISM Data
• Fluid Dynamics of Local Martian Magma Oceans: Implications for Hemispherical Dichotomy and Tharsis Formation
• Formation of Lower Mantle Heterogeneity due to Grain Size-Dependent Viscosity
• Geochemical Constraints on Archaeal Diversity in the Vulcano Hydrothermal System
• Geophysical implications of reduction in thermal conductivity due to hydration
• High-Precision Fe Isotope Measurements of the 3.7-3.8 Ga Isua Banded Iron Formation
• High-temperature measurements of olivine thermal diffusivity
• Lunar Science for Future Missions
• MARSIS Subsurface Sounding Observations of the Polar Deposits of Mars
• Mars Mineralogy from OMEGA Visible-Near Infrared Measurements
• Mars Reconnaissance Orbiter: An Overview of Early Results and Plans for Further Observation
• Microbe-Mineral Interactions in Extinct Hydrothermal Chimneys at East Pacific Rise: Molecular and Microscopic Approaches
• Microbe-Mineral Interactions in Extinct Hydrothermal Chimneys at East Pacific Rise: Spatially-Resolved Chemical and Mineralogical Approaches
• Microbial Geochemistry in Shallow-Sea Hydrothermal Systems
• On Sister, Where Art Thou? The Galilean Satellites After Galileo
• Photometric Analysis of Olivine and Pyroxene Using Hapke Modeling
• Remote Detection and Monitoring of Glacial Slip from Whillans Ice Stream using Seismic Rayleigh Waves Recorded by the TAMSEIS Array
• Results for the Mantle Transition Zone Beneath the Transantarctic Mountains From Receiver Functions
• Rheology as Master of the Satellite Universe (Geophysical Modeling of Ice-Rock Bodies)
• Rock Rinds at Meridiani and Surface Weathering Phenomena
• Sediment dynamics and the changing nature of the subduction component beneath the Kurile volcanic Arc
• Seismic Attenuation Structure of the Mariana Subduction System
• Seismicity of the Mariana Shallow Thrust Zone From Ocean Bottom Seismograph Observations
• Silicious Biofilms in Alkaline Geyser Basins of Yellowstone National Park
• Spectral Diversity of Rock Fragments at the Meridiani Planum Landing Site
• The Composition of Soils at Gusev Crater, Mars as Measured by Mini-TES: Sulfates, Basaltic-Sand, and Dust
• The May 3, 2006 (Mw 7.9) Tonga Earthquake: Shallow Thrust or Slab Tear? Evidence From Locally Recorded Aftershocks
• Thermal diffusivity of spinels at elevated temperature: implications for heat transfer in the transition zone
• Thermophysics During the MER Spirit Winter Campaign: Observing Complex Surfaces Through Seasonal and Diurnal Cycles
• Trench-Parallel Flow in the Mariana Mantle Wedge: Comparisons of Shear-Wave Splitting and Numerical Models of Mantle Flow
• Two-dimensional seismic velocity model of the upper crust at SAFOD from multi-offset VSP and refraction data
• Upper Mantle Structure Beneath the Cameroon Volcanic Line From Preliminary Body-wave Tomography
• Viscoelastic Relaxation of Tidally Induced Stresses in the Ice Shells of Outer Solar System Satellites
• A Study of the Subsurface Structure of a Region of the Martian South Polar Layered Deposits by Means of Sharad High Resolution Radar Data
• An Overview of MARSIS and SHARAD Radar Sounding Observations of the Polar Deposits of Mars
• Attenuation Tomography of Western North America Using USArray Body Waves
• CRISM Retrieval of Surface Lambert Albedos for Multispectral Mapping of Mars with DISORT- based Radiative Transfer Modeling: Phase 1 -- Using Historical Climatology for Temperatures, Aerosol Optical Depths, and Atmospheric Pressures
• Chemistry of Earth's Putative Steam Atmosphere
• Cold Fire: The Geology and Geophysics of Enceladus
• Coupled core-mantle thermal evolution after a giant impact
• Density of Mars' South Polar Layered Deposits
• Detailed Structure of Upper Mantle Discontinuities in the Tonga and Mariana Subduction Zones
• Evidence for a Possible Siliceous Sinter Deposit at Home Plate in Gusev Crater
• High Field Strength and Rare Earth Element Systematics of the Kurile arc.
• Imaging Lower Mantle Heterogeniety With Differential Dispersion and Attenuation of Core- Diffracted Waves
• Implications for backarc basin dynamics including a low viscosity wedge in simple 2 and 2.5D numerical flow models
• Incoherent Simulator for Mars Surface Applied to the Analysis of Sharad Radar Data
• Investigating the Wavelength Dependence of the Single-Scattering Albedo of Martian Dust Aerosols with CRISM and MARCI Observations of the Very Dusty Atmosphere in 2007
• Juxtaposition of Layered Sulfate and Phyllosilicate Deposits, Meridiani Planum, Mars
• Mantle Structure, Melting and Flow in the Nicaragua-Costa Rica and Izu Bonin-Marianas Subduction Zones
• Mapping and Characterization of the Eastern Elysium Planitia Deposits
• Mars early geological and climatic evolution, derived from its surface mineralogy
• Mars: South Polar Spring Recession as observed by CRISM
• Microseismicity in the Lau Basin from T-phases recorded by the LABATTS ocean bottom seismograph experiment
• Multi-sulfate and Iron Oxide Assemblages Within the Valles Marineris Interior Layered Deposits
• Observations of Shallow Thrust Seismicity in the Northern Mariana Subduction Zone From Broadband Ocean-bottom and Land Seismometers
• P- and S-wave Tomography of the Cameroon Volcanic Line Used to Discriminate Between Formation Models
• POLENET: Polar Earth Observing Network for the International Polar Year
• Radar Subsurface Sounding Over the Putative Frozen Sea in Cerberus Palus, Mars
• Rayleigh Wave Phase Velocity Structure of the Cameroon Volcanic Line Region
• Reproducibility of Raman Spectroscopy Measurements for Carbonaceous Material in Metamorphic Rocks
• Results From the SHARAD Sounding Radar Experiment at Mars
• SHARAD radar stratigraphy of the Martian North Pole
• Seismic Evidence for Widespread Serpentinized Forearc Mantle Along the Mariana Convergence Margin
• Simultaneous GPS and teleseismic monitoring of glacial stick-slip of Whillans Ice Stream, West Antarctica.
• Spectral Mapping of Interior Layered Deposits of Western Candor Chasma by CRISM
• Temperature-Dependent Thermal Diffusivity of Crustal Minerals, Rocks and Melts: Implications for Positive Thermal Feedback During Crustal Anatexis
• VEIL: A New Frontiers Class Mission Concept for Exploring Venus
• Wind-Driven Particle Mobility on Mars: Insights from MER Observations
• Ambient Noise Rayleigh Wave Tomography in Antarctica From the TAMSEIS Array
• Carbon Sequestration and Nitrous Oxide Emissions from Urban Turfgrass Ecosystems in Southern California
• Crustal Structure Along the Transantarctic Mountain Front Using Receiver Functions
• Crustal Structure in Cameroon From Receiver Function Analysis
• Crustal Thickness and Vp/Vs Beneath the Florida to Edmonton Broadband Seismometer Array
• Earth Science Literacy: Building Community Consensus
• Environmental Implications of Ediacaran C-isotopic Shifts
• Exploring Earth's Lowermost Mantle With Core-Diffracted Waves From Linear Arrays
• Ferric sulfates on Mars: Surface Explorations and Laboratory Experiments
• Geochemical Energy for Catabolism and Anabolism in Hydrothermal Systems
• Geologic Context of Al-rich Phyllosilicate Deposits in Meridiani
• High-Silica Rocks and Soils at Gusev Crater, Mars: Distribution, Spectra, and Implications for Past Hydrothermal Activity
• Mass-independent isotopic fractionation of tin in a chemical exchange reaction
• Pancam Spectral Variations Across Home Plate: Bonestell Panorama, Gusev Crater, Mars
• Preliminary identification of minerals at the Mars Phoenix Landing Site
• Properties of Martian Dust Aerosols From the Combination of MER and MGS/MRO Observations
• Regional Body-wave Tomography Reveals a Linear Deep-seated Low-velocity Zone Beneath the Cameroon Volcanic Line
• Regional Crustal Velocity Models for Northern Arabian Platform and Turkish-Iranian Plateau
• Seismic Constraints on Water Cycling Through the Mantle
• Shear Velocity Structure of the Cameroon Volcanic Line Region from Rayleigh Wave Phase Velocities
• Size-Frequency Distribution of Rock Clasts at the Phoenix Landing Site
• Spectral Modeling of Ground Ices Exposed by Trenching at the Phoenix Mars Landing Site
• Subsurface Materials Exposed at the Phoenix Landing Site
• Subsurface Structure of Planum Boreum on Mars from Shallow Radar (SHARAD) Soundings
• Sulfates and Other Hydrated Minerals in Ius Chasma, Valles Marineris and Implications for Water Geochemistry
• Sulfur- and Oyxgen(?)-Rich Cores of Large Icy Satellites
• Surface Properties and Characteristics of Mars Landing Sites from Remote Sensing Data and Ground Truth
• Terrestrial constraints on the timing and magnitude of Saharan humid phases
• The Biogeochemistry and Ecology of Deep Sediment-Buried Basement Biosphere: Juan de Fuca Ridge Flanks
• The role of groundwater in the origin of the indurated layered deposits of Arabia Terra, Mars
• Time-Dependent SSI Multispectral Properties for Rock, Soil, Ice, and Sublimation Lags at the Phoenix Landing Site on Mars
• A LATE BRITTLE COMPONENT OF MOTION WITHIN THE DUCTILE EASTERN SIERRA CREST SHEAR ZONE (ESCSZ) ALONG THE EASTERN BOUNDARY OF THE TOLUMNE BATHOLITH IN THE SADDLEBAG LAKE, CA AREA. WHITESIDES, Andrew1, ENRIQUEZ, Marcus2 , HARDY, Jill1 , EHRET, Philip1, IANNONE, Monika1, CULBERT, Kristan1 GROSS, Ben3, LODEWYK, Jessica3, CAO, Wenrong1 , ZHANG, Tao1, MEMETI, Valbone3, PATERSON, Scott1 SCHMIDT, Keegan4. (1) Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, awhitesi@usc.edu , (2) Department of Geological Sciences, Cal State L.A., 5151 State University Drive, Los Angeles, CA 90032, (3) Department of Earth and Planetary Sciences, Washington University, Campus Box 1169, 1 Brookings Dr, Saint Louis, MO, 63130, (4) Division of Natural Science and Mathematics, Lewis-Clark State College, 500 8th Ave., Lewiston, ID 83501
• A Survey of Earth's Lowermost Mantle Utilizing Core-Diffracted Waves
• Archaea, Bacteria, and Sulfur-Cycling in a Shallow-Sea Hydrothermal Ecosystem
• Building Community Consensus for Earth Science Literacy Using an Online Workshop (Invited)
• CRUSTAL TECTONICS AND SEISMICITY OF THE MIDDLE EAST
• Constraining Formation Models for the Cameroon Volcanic Line Using Broadband Seismic Data
• Crust and Upper Mantle Shear Wave Structure of Antarctica From Seismic Ambient Noise
• Determination of absolute arrival times for secondary phases from combined waveform cross-correlation and differential t* measurement: Application to USArray data
• Europa: Perspectives on an Ocean World
• Evaluating the Role of Small Impoundments in Legacy Sediment Storage
• Evidence for Unconformable Deposition of Hydrated Sulfate-bearing Evaporitic Deposits in Northern Sinus Meridiani, Mars
• Examining the role of magma mixing with major and minor element distribution patterns in rock-forming minerals in the Tuolumne batholith, Sierra Nevada, CA
• Exploration Strategy for the Ice Dwarf Planets 2013-2022
• Intermediate depth double seismic zone and serpentine dehydration in subducting oceanic lithosphere beneath the Northern Mariana Islands from ocean bottom seismograph observations
• Interpreting Al-in Hornblende and Hbl-Plag thermobarometry results from the Tuolumne batholith and magmatic lobes in conjunction with single mineral element distribution electron microprobe maps
• LRO Camera Imaging of Constellation Sites
• LRO Camera Imaging of the Moon: Apollo 17 and other Sites for Ground Truth
• LROC Observations of Geologic Features in the Marius Hills
• Landscape change and sediment yield of rivers in the northeastern US during 19th century
• Mapping the Moon with LROC: Global ultraviolet through visible color observations
• Microstructural evolution in coarse grained dunite deformed to large strains
• Recent Spirit Rover Results: Morphological and Textural Analysis of Sulfate-Rich Soils to the West of Home Plate
• Recommended Exploration Strategy for the Outer Planets 2013-2022: Goals and Priorities
• Regional lead dynamics in the Northeastern United States - Local versus regional industrial influences
• Response of Robust Torsion Balances to Teleseismic Events
• Seismic Anisotropy Beneath the Cameroon Volcanic Line from SKS and SKKS Splitting Analysis
• Seismic Anisotropy of the Antarctic Upper Mantle from Shear Wave Splitting Analysis of POLENET and AGAP Seismograms
• Seismic structure of the Gamburtsev Mountains, East Antarctica and surrounding regions from surface wave tomography
• Spectral and Textural Changes Observed in Sulfate Soil Deposits at Gusev Crater, Mars
• Structure of the Crust Beneath Cameroon (West Africa) From the Joint Inversion of Rayleigh Wave Group Velocities and Receiver Functions
• Super-heavy pyrite (δ34Spyr &gt; δ34SCAS) in the terminal Proterozoic Nama Group, Southern Namibia: Implications for atmospheric oxygen and seawater sulfate at the dawn of animal life
• Technologies for Outer Planet Missions: A Companion to the OPAG Exploration Strategy
• The 2009 Earth Science Literacy Principles
• The Invisible Heat: Heat-Production By Strain In The Continental Crust
• The L-SCAN Seismic Tomography and Geophysical Mapping Experiment
• The historical effects of coal mining on the hydrology of Appalachia
• Thermal Diffusivity of Magmas: Implications for Heat Transport in Partially Molten Zones
• Using S-wave Receiver Functions to estimate crustal structure beneath ice sheets: an application to the Transantarctic Mountains, the Gamburtsev Mountains, and the East Antarctic Craton
• Variations in soil properties at the Phoenix Landing Site
• A Lipid Biomarker Stratigraphic Record through the Late Ordovician Mass Extinction
• A dominant shear zone and other modes of deformation in the deep Tonga slab
• Along-strike Changes in Plate-bending Seismicity in the Mariana Islands: Implications for Strength of Interplate Coupling and Hydration of the Subducting Pacific Slab
• Average Hapke parameters of the surface traversed by the Opportunity rover at Meridiani Planum, Mars
• Battlefield Seismology from Baghdad, Iraq
• Complexity of Arsenate Adsorption at Iron and Aluminum Oxide-Water Interfaces
• Constraints on the duration and magnitude of Late Ordovician-Early Silurian glaciation and its relationship to the Late Ordovician mass extinction from carbonate ``clumped'' isotope paleothermometry
• Crustal Structure of the Gamburtsev Mountains, East Antarctica, from S-wave Receiver Functions and Rayleigh Wave Phase Velocities
• Degassing of CO2 from headwater streams as a Rayleigh process
• Detection of Seismic Sources Associated with Ice Movement in Antarctica using the AGAP and POLENET Seismic Deployments
• Earth and Space Science in the new NRC "Conceptual Framework for New Science Education Standards"
• East Antarctic Seismic Anisotropy from Shear-wave Splitting Analysis of AGAP Seismograms
• Experimental deformation of natural dunite: Effects of suppressed diffusion creep on microstructural evolution
• Flux rates and sulfur isotopic composition of pore fluids from three mud volcanoes in the northern Gulf of Mexico
• Generating topography through tectonic deformation of ice lithospheres: Simulating the formation of Ganymede's grooves
• Hydroacoustic Monitoring of Seismic and Volcanic Activity within the Lau Basin (Invited)
• Lithospheric S-velocity structure of Antarctica inverted from surface waves
• New Constraints on Archean Sulfur Cycling from the Spatial Variability of Mass-Dependent and Mass-Independent Isotopic Signatures
• On the geographic and stratigraphic variability of the Hirnantian positive carbon isotope excursion across Anticosti Island, Canada
• Organic chemistry of fluids from sediment-buried young basement: discrete sampling from ODP borehole 1301A &amp; 1025C
• Origin of microseisms in equatorial and southern Africa from analysis of broadband arrays
• Photometric Properties of Phobos Derived from CRISM and OMEGA Observations
• Pioneering Techniques to Determine Wastewater and Urban Runoff Loads in Karst Spring Systems
• Radiogenic Argon Release from Titan: Sources, Efficiency, and Role of the Ocean (Invited)
• Receiver functions on ice: crust and mantle properties from POLENET
• Retrieval and Interpretation of 0.4 to 4.0 μm Lambert Albedos over Aram Chaos from Mars Express OMEGA Data
• Saline Playas on Qinghai-Tibet Plateau as Mars Analog for the Formation-Preservation of Hydrous Salts and Biosignatures
• Temperature-dependent thermal transport properties of Archean rocks
• Testing Planetary Radiative Transfer Models via Remote Sensing of Gypsum Sands in White Sands National Monument
• The Weirdest Topography in the Outer Solar System: The Ridge on Iapetus and its Possible Formation via Giant Impact (Invited)
• Upper Mantle Structure Beneath the Gamburtsev Subglacial Mountains, East Antarctica via Body-Wave Tomography
• Using mineral thermal diffusivities measured with Laser-Flash Analysis to redefine the continental geotherm
• Velocity Structure of the Lowermost Mantle Beneath the Northeast Pacific From Core-Diffracted P and S Waves
• Why Can't Mimas Be More Like Enceladus?
• Window into Sediment-Buried Basement Biosphere: Fluid Sampling from CORK Observatory Seafloor Platforms, Juan de Fuca Ridge Flanks
• Analysis of Along-Track Oversampled CRISM Observations
• Analysis of Core-Diffracted P &amp; S Waves from Station-Pair Profiles
• Arsenic metabolism by microbial communities from an arsenic-rich shallow-water hydrothermal system in Ambitle Island, Papua New Guinea
• Atmospheric Formation of Rocky Terrestrial Planets
• CRISM-Derived Spectral Scattering Parameters for Surfaces in the Vicinity of Opportunity Mars Rover Traverses
• Characterization of Phyllosilicates by LIBS and Laser Raman Spectroscopy
• Clay Formation Dominantly in the Subsurface? Implications for Early Mars Environments
• Comparing Rover and Orbiter based observations at Meridiani Planum, Mars
• Control of Thermal Diffusivity by Infrared Optical Modes: Theoretical and Geophysical Implications
• Coordinated CRISM and Opportunity Observations to Characterize the Mineralogy and Geologic History of Meridiani Planum Outcrops
• Coordinated CRISM and Opportunity Observations to Characterize the Mineralogy and Geologic History of Smectite-Bearing Noachian Outcrops on the Cape York Rim Segment of Endeavour Crater
• Developing New Earth and Space National Science Standards
• Dust Accumulation on MER Solar Panels
• Ediacaran ocean chemistry: Insights from multiple sulfur isotope measurements of paired sulfate- pyrite in the Huqf Supergroup, Oman
• Evidence for hydrological changes in far-field seismic waveforms from Whillans Ice Stream fast slip events
• Experimental Reactivation of Pseudotachylite-bearing Faulted Rocks
• Hydrated Minerals Associated with Interior Layered Deposits near the Southern Wall of Melas Chasma, Valles Marineris, Mars
• Interior of Titan: 2-Layer or 3-Layer and Does It Matter?
• Martian Seasonal CO2 Frost Indicating Decameter-Scale Variability in Buried Water Ice
• Microstructural evolution of experimentally deformed harzburgites
• Mineral-Water Interface Processes Affecting Uranium Fate in Contaminated Sediments
• On the Cutting Edge: Face-to-Face and Virtual Professional Development for Current and Future Geoscience Faculty
• Origin of Aristarchus Olivine Deposits Based on M3, WAC, and Diviner Analyses
• Origin of Axial Spin and Orbital Rotation of the Solar System
• Oxidative Transformations of Ferrous Iron-Bearing Smecitites: Routes to Martian Nontronites
• Seismic Noise Levels Across Antarctica
• Spatial heterogeneity in sulfur isotopes: implications for modern environments and paleoenvironmental reconstructions
• Subduction zone plate bending earthquakes and implications for the hydration of the downgoing plate
• Sulfur isotope systematics of microbial mats in shallow-sea hydrothermal vents, Milos Island, Greece
• The Relationship of Intermediate- and Deep-Focus Seismicity to the Hydration and Dehydration of Subducting Slabs
• The search for arsenotrophs in the arsenic-rich marine shallow-water hydrothermal system off Milos Island, Greece
• Thermal Emission Spectra of Post-Giant-Impact Earths
• Thermal History and Crystallinity of Sheet Intrusions
• Thermodynamic Predictions of Phyllosilicate Assemblages Produced under Mars-Relevant Weathering and Alteration Scenarios
• Tools and Methods for Visualizing and Representing Seismic Waves in College Classrooms
• Traces on the 'Ubaidian Shore: Mid-Holocene Eustasis, Marine Transgression, and Urbanization in the Mesopotamian Delta (Iraq)
• Tracking the Effect of Sea Ice Cover on Microseismic Noise Using Two Seismic Arrays in Antarctica
• Two-Stage Deformation of Olivine Aggregates with Changing Deformation Kinematics
• Was the September 3 2010 Mw 7.1 Darfield, New Zealand Earthquake Triggered by the 2009 July 15 MW 7.8 Dusky Sound, New Zealand Earthquake, 500 km Away?
• Zn and C isotopic evidence of climatic change during the Marinoan
• Zn isotopic composition of planetary basalts
• Zones of life in the subsurface of hydrothermal vents: A synthesis
• 3D Lithosphere structure of the Antarctic plate and its implications on the plate evolution
• A thermodynamic and mechanical model for the earliest Solar System: Formation via 3-d collapse of dust in the pre-Solar nebula
• Argon Concentrations of Fine-Grained Marine Sediments near Wilkes Land, Antarctica: Source Characterization and Implications for Ice Sheet Behavior during the Middle Miocene
• Crust and Upper Mantle Structure of Antarctica from Rayleigh Wave Tomography
• Earth's interdependent thermal, structural, and chemical evolution
• Effect of variable hydrothermal conditions on sulfur speciation and isotopic compositions mediated by two Thiomicrospira strains
• Estimates of Crustal Structure in Antarctica from S-Wave Receiver Functions
• Facies variability in the post-Marinoan cap carbonate Nuccaleena Formation on the Stuart Shelf, South Australia
• Geochemical analysis of layered outcrops using laser-induced breakdown spectroscopy (LIBS) - Implications for Mars exploration
• Hematite Bearing Ridge as Evidence for Anoxic Water Discharge in Gale Crater
• Identification of phyllosilicates and sulfates near the southern wall of Melas Chasma on Mars
• Imaging Mantle Melting Beneath Island Arcs and Backarc Spreading Centers
• Implications of the Next Generation Science Standards for Earth and Space Sciences
• In Situ Observational Constraints on GIA in Antarctica
• Influence of Nonhydrostatic Cores on the Shapes of Icy Satellites such as Enceladus: Implications for Internal Structure, Gravity, and Survival of its Subsurface Ocean
• Investigating Mantle Structure with Broadband Seismic Arrays in Madagascar and Mozambique
• Iron Isotopic Fractionation in Early Planetary Crusts
• Micron-scale Analysis of Carbonate-Associated Sulfate by Secondary Ionization Mass Spectrometry: Insights into Spatial Variability in δ<SUP>34</SUP>S<SUB>CAS</SUB>
• New estimates of subducted water from depths of extensional outer rise earthquakes at the Northwestern Pacific subduction zones
• Olivine LPO and the interpretation of seismic anisotropy in the upper mantle
• Preservation of Subsurface Sulfates with mid-to-high degree of hydration in Equatorial regions on Mars
• Reconciling geophysical and geochemical observations to understand craton lithosphere architecture
• Seismic attenuation tomography of the Tonga Arc and Lau Backarc Spreading Center
• Shear Velocity Structure of the Tonga Arc and Lau Backarc Basin from Rayleigh Wave Tomography
• Source characteristics of a West Antarctic ice stream
• Spatial isotopic heterogeneity during the Guttenberg isotopic carbon excursion: Mechanisms and implications for craton-wide isotope gradients
• Subglacial volcanic seismicity in Marie Byrd Land detected by the POLENET/ANET seismic deployment
• The Transition from Phyllosilicate to Hydrated Sulfate Deposition as Evidenced from Mars Reconnaissance Orbiter CRISM and Opportunity Rover Observations in Meridiani Planum
• The impact of sediment remobilization on lateral and vertical heterogeneity in the sulfur isotopic composition of pyrite (δ<SUP>34</SUP>S): a case study from the Gulf of Papua deltaic complex
• The influence of water on the formation of mantle shear zones
• The silicon isotope composition of enstatite meteorites and their importance as proto-Earth components
• The upper mantle shear wave velocity structure of East Africa derived from Rayleigh wave tomography
• Traces of extension in continental lithosphere: Towards a seismic image of the Mid-Continent Rift
• Understanding Uranium Behavior in a Reduced Aquifer
• Upper mantle phase velocity and shear wave velocity structure beneath the Cameroon Volcanic Line region
• Upper mantle shear velocity structure beneath Eastern Lau back-arc Spreading Center from ambient noise tomography of ocean bottom seismometer data
• 3-D Distribution of Partial Melt beneath the Lau Backarc Basin from Seismic Attenuation Tomography
• Analysis of the Mantle Transition Zone beneath West Antarctica using P-wave receiver functions
• Arsenic Scavenging by Al-Substituted Ferrihydrites in a Circumneutral pH River Impacted by the Acid Mine Drainage of Carnoulès, Gard, France
• Assessing Water Management of Mining Effluent Using Temporal and Spatial Hydrologic Analyses: The Case of QIT Madagascar Minerals
• Biogeochemistry of Stinking Springs, UT Part I: Inorganic carbon dynamics and constraints on nutrient fluxes in a warm, salty, sulfidic spring
• Biogeochemistry of Stinking Springs, Utah. Part II: Microbial Diversity and Photo- and Chemo-Autotrophic Growth Rates in a Layered Microbial Mat
• Biogeochemistry of the sulfur oxidizer Thiomicrospira thermophila
• Cenozoic extension, volcanism and plateau uplift in eastern Africa and the African Superplume
• Clues to the formation of Enceladus' south-polar terrain from simulations of funiscular plains formation
• Comparing the Chemistry for the Pathfinder, MER and MSL Martian Landing Sites with APXS
• Comprehensive Study of the Crust and Upper Mantle within East and West Antarctica Based on S-wave Receiver Functions
• Depth variation of upper mantle seismic discontinuities in the region of the Tonga subduction zone
• Diazotrophy in the Deep: Measuring Rates and Identifying Biological Mediators of N<SUB>2</SUB> fixation in Deep-Sea Sediments
• Effects of deformation history on texture evolution in experimentally deformed Åheim dunite
• Enriched Pyrite δ34S Signals in Modern Tropical Deltaic Muds
• GPS observations of glacial isostatic adjustment into the Antarctic Interior
• Grounding line control of rupture initiation and propagation during Whillans Ice Stream slip events (Invited)
• High-frequency Seismic Signals in Antarctica Triggered by the 2010 Mw8.8 Maule, Chile Earthquake
• How Climate Science got to be in the Next Generation Science Standards (Invited)
• In Situ <SUP>13</SUP>C NMR at Elevated-Pressures and -Temperatures Investigating the Conversion of CO<SUB>2</SUB> to Magnesium and Calcium Carbonate Minerals
• Investigating the effects of abyssal peridotite alteration on Si, Mg and Zn isotopes
• Is Enceladus' Internal Ocean Doomed to Freeze?
• Mars Exploration Rover Opportunity Mobility Simulation of Traverses at Endeavour Crater, Mars
• New CRISM Along-Track Oversampled Observations and Implications for Spectral Mapping at Fine Spatial Scales
• Origin of isotopically light Zn in lunar samples through vaporization and the Zn isotope composition of the Moon
• Parametric study of the factors affecting wheel slip and sinkage for the Mars Exploration Rovers
• Preliminary Results for Crustal Structure in Southeastern Africa from P-wave Receiver Functions
• Probing the Extremes in the Water-Ice Content of the Martian Permafrost
• ROV Hyper-Dolphin Survey at the May 2010 Eruption Site on South Sarigan Seamount, Mariana Arc
• Receiver function analysis and preliminary body wave tomography of the MACOMO network in Madagascar
• Recovery and Restoration of Apollo Lunar Surface Experiments Package (ALSEP) Data by the NSSDC and the PDS Lunar Data Node
• Secondary Craters and the Size-Velocity Distribution of Ejected Fragments around Lunar Craters Measured Using LROC Images
• Seismic constraints on mantle hydration during subduction: Mariana versus Middle America Trench
• Silicon and Zinc Isotopes in Ocean Island Basalts
• Source and Aftershock Analysis of a Large Deep Earthquake in the Tonga Flat Slab
• Teaching About Critical Earth Issues in the 2U Semester Online Consortium (Invited)
• The 'Nuts and Bolts' of <SUP>13</SUP>C NMR Spectroscopy at Elevated-Pressures and -Temperatures for Monitoring In Situ CO<SUB>2</SUB> Conversion to Metal Carbonates
• The Lassell Massif - a Silicic Lunar Volcano
• The nature of Earth's building materials as revealed by calcium isotopes
• The role of phase mixing in shear localization in the mantle
• The structure of the mid-continent rift of North America from combined surface wave and ambient noise tomography
• Three dimensional crust and upper mantle velocity structure of Antarctica from seismic noise correlation (Invited)
• Tourmaline in the 3.7-3.8 Ga Isua Supracrustal Belt, West Greenland - A window to Boron Concentrations in the Eoarchean Eon
• Towards scaling laws for subduction initiation on terrestrial planets: Constraints based on single-cell steady-state convection simulations
• Upper mantle velocity structure beneath the Cameroon Volcanic Line region and implications for the formation of mantle hot lines
• Validation of Artemis Mobility Simulations for the Spirit, Opportunity, and Curiosity Mars Rovers
• Variable quartz lattice preferred orientation patterns within a mylonite from the Rockfish Valley Shear Zone of the Central Virginia Blue Ridge
• A New Method to Minimize the Influence of Lateral Heterogeneity on Inversion Applying Triplicated Phases
• Applications of Subspace Seismicity Detection in Antarctica
• Assessing Microseismicity of the Northern Mid-Continent Rift Zone and Surrounding Regions
• Combined teleseismic surface wave and receiver function analysis of the crust and upper mantle of Madagascar
• Crustal Structure of and near the North American Mid-continent Rift System from Receiver Function Studies
• Depth Variation of Upper Mantle Seismic Discontinuities in the Region of the Tonga Subduction Zone
• Detection of Repeating Earthquakes Along the Northern Mariana Shallow Thrust Zone
• Effects of Seasonal and Secular changes in Antarctic Sea Ice on Microseismic Noise
• Evidence from P-wave receiver functions for lower mantle plumes and mantle transition zone water beneath West Antarctica
• Fault Mirror Formation and Destruction Correlates With Slip Rates on Carbonate Faults
• GPS Measurements of Crustal Motion Indicate 3D GIA Models are Needed to Understand Antarctic Ice Mass Change
• Gravitational signature and apparent mass changes in Amundsen Embayment caused by low viscosity GIA model constrained by rapid bedrock displacement
• Mercury's Hollows: New Information on Distribution and Morphology from MESSENGER Observations at Low Altitude
• SPREE: A Successful Seismic Array by a Failed Rift System; Analysis of Seismic Noise in the Seismically Quiet Mid-continent
• Seismic Velocity and Attenuation Tomography of the Tonga Arc and Lau Back-arc Basin
• Seismic structure of the Tonga Arc and Lau Backarc Spreading Center from joint inversion of local and teleseismic body wave arrivals
• Seismicity of the Incoming Plate at the Mariana Trench Located Using an Ocean Bottom Seismograph Array
• Shear Velocity Structure of the Crust and Uppermost Mantle across the Mariana Trench from Ambient Seismic Noise
• Shear Wave Splitting Across Eastern, Western and Southern Africa
• Strong Seismic Scatterers Near the Core-Mantle Boundary North of Pacific Anomaly From PKP Precursors Recorded by Antarctica Arrays
• Teleseismic P-wave Delay Time Tomography of the southern Superior Province and Midcontinent Rift System (MRS) Region
• The Crust and Mantle Structure of the Mid-Continent Rift System from Ambient Noise and Earthquake Surface Wave Analysis
• The Effect of Recent Volcanic Activity on the Seismic Structure of Madagascar
• The effect of deformation history on the texture and seismic anisotropy of the upper mantle: Results from experiments and numerical modeling
• Basal Conditions in Marie Byrd Land in the Presence of a Deep Mantle Plume
• Characterizing Amorphous Silicates in Extraterrestrial Materials
• Creep Parameterization for the 3-D Mantle: Implications for Geodetic Interpretations of GIA
• Crust Uppermost Mantle Structure beneath Eastern Asia: Progress towards a Uniform, Tightly Constrained, High Resolution 3-D Model
• Crustal Structure in the area of the North American Mid-Continent Rift System from P-wave Receiver Functions
• Crustal and Uppermost Mantle Shear Velocity Structure across the Mariana Trench
• Gravitational signature and apparent mass changes in Amundsen Embayment caused by low viscosity GIA model constrained by rapid bedrock displacement
• Ice shelf structure from dispersion curve analysis of passive-source seismic data, Ross Ice Shelf, Antarctica
• Infrasound and Seismic Recordings of a US Airstrike on an ISIS Car Bomb Factory on June 3, 2015
• Investigating the possibility of East Antarctic ice mass loss as an explanation for GPS-derived observations of horizontal motion
• Mantle Flow Implications across Easter and Southern Africa from Shear Wave Splitting Measurements
• Mercury's Hollows: Depths, Estimation of Formation Rates, and the Nature of the Bright Haloes
• North America's Midcontinent Rift: when Rift MET Lip
• Ocean-Based Seismic Noise Sources Recorded by a Moderate Aperture Array in Antarctica
• Pathway Study of Cl-cycle on Mars, Step-I &amp; II: Oxychlorine Salts and Electrostatic Discharge Phenomenon in a Mars Chamber
• Prolific Sources of Icequakes: The Mulock and Skelton Glaciers, Antarctica
• Rayleigh Wave Tomography of Mid-Continent Rift (MCR) using Earthquake and Ambient Noise Data
• Seismic Constraints on Water and Melt Pathways and Fluxes Through Island Arc System
• Seismic Excitation of the Ross Ice Shelf by Whillans Ice Stream Stick-Slip Events
• Sources of Melt beneath the Lau Back Spreading Center and Tonga Arc as Indicated by Local and Teleseismic Bodywave Tomography
• Teleseismic Body Wave Analysis of the Madagascan Asthenosphere, and the Relationship to Intraplate Volcanism
• Teleseismic Earthquake Signals Observed on an Ice Shelf
• The Seismic Structure of the Crust of Madagascar
• The crustal thickness and lithospheric structure of active and inactive volcanic arc terrains in Fiji and Tonga
• The effect of deformation history on the interpretation of seismic anisotropy in the upper mantle: experiments and numerical modeling
• The intermediate-depth Tonga double-seismic zone and relationship to slab thermal structure
• Understanding the Physical Causes of Surface Wave Amplitude Variations across Eastern Asia through Seismic Waveform Simulation
• A New Approach to the Visual Rendering of Mantle Tomography
• A reference model for crust and uppermost mantle beneath Antarctica
• Advances in Solid Earth and Basal Water Dynamics and their Relation to GIA in Antarctica
• Assessing the Provenance of regolith components in the South Pole-Aitken Basin: Results from LRO, M<SUP>3</SUP>, GRAIL, and Ejecta Modeling
• Chacterization of Teleseismic Earthquakes Observed on an Ice Shelf
• Chilean Tsunami Rocks the Ross Ice Shelf
• Constraints on Mantle Serpentinization near the Mariana Trench from Earthquake and Ambient Noise Rayleigh Waves
• Constraints on the variable subglacial structure of Whillans Ice Stream from ambient noise Rayleigh wave H/V ratios
• Contrasts in Lower Crustal Structure and Evolution Between the Northern and Southern Rocky Mountains From Xenoliths and Seismic Data
• Crustal structure beneath seismic stations deployed on rock in West Antarctica: New constrains on crustal shear wave velocities, Poisson's ratios and Moho depths
• East Antarctic intraplate earthquakes recorded by the AGAP/GAMSEIS temporary seismic array delineate possible ancient rift
• Energy Dissipation and Fault Slip Kinematics: Effects of Velocity History
• Flexural-gravity Wave Attenuation in a Thick Ice Shelf
• Full Waveform Adjoint Seismic Tomography of the Antarctic Plate
• High-resolution Body Wave Tomography of the Ross Sea Embayment, Antarctica
• Incoming Plate Seismicity of the Northern Mariana Trench Recorded by Ocean Bottom Seismographs and Implications for Slab Hydration
• Insights into Along Strike Variability in the Lau Back Spreading Center and Tonga Arc from Bodywave Tomography
• Modification of olivine CPO during high temperature annealing
• Recent Opportunity Microscopic Imager Results from the Western Rim of Endeavour Crater
• Sea-Level Fingerprints in a Region of Complex Earth Structure: the Case of WAIS
• Structures Within the South Polar Cap of Mars from Three-dimensional Radar Imaging
• The Lithospheric Structure of Madagascar
• The Long-Standing Antarctic Mantle Plume Hypothesis and Modeling Ongoing Glacial Isostatic Adjustment
• Two-Oxide Disequilibrium: A New Geospeedometer Based on Diffusion in Ilmenite
• Upper mantle seismic anisotropy and the evolution of olivine crystallographic preferred orientation
• Xe isotopic constraints on deep volatile cycling over Earth history
• Archiving InSight Lander Science Data Using PDS4 Standards
• Cassini Ion Mass Spectrometer Peak Calibrations from Statistical Analysis of Flight Data
• Climate Implications of an Ancient Lake Basin in Gale Crater, Mars
• Developing an Augmented Reality Environment for Earth Science Education
• Distributions of high-velocity lower crust and seismic anisotropy across the continental U.S.: Integration of seismic, xenolith, and surface geologic data to address lithospheric dynamics and history
• Exploring Planetary Analogs With an Ultracompact Near-Infrared Reflectance Instrument
• Formation of the Lunar Fossil Bulges and its Implication for the Early Earth and Moon
• High-Resolution Body Wave Tomography of the Ross Sea Embayment, Antarctica
• Hydrogen isotopic messages in sulfate reducer lipids: a recorder of metabolic state?
• Linking Incoming Plate Faulting and Intermediate Depth Seismicity
• Mantle Serpentinization near the Central Mariana Trench Constrained by Ocean Bottom Surface Wave Observations
• Normal-Faulting in Madagascar: Another Round of Continental Rifting?
• One billion year-old Mid-continent Rift leaves virtually no clues in the mantle
• Orbital and Rover-based Exploration of Perseverance Valley, Endeavour Crater, Mars
• P-wave Velocity Structure Across the Mariana Trench and Implications for Hydration
• Portrayal of the Geosciences in the New York Times
• Repeating earthquakes and subglacial conditions.
• Seismic and thermal structure of the crust and uppermost mantle beneath Antarctica from inversion of multiple seismic datasets
• The Role of NASA's Planetary Data System in the Planetary Spatial Data Infrastructure Initiative
• Understanding the Underground Hydrous Minerals on Mars: Stability Field, Phase Transitions, and Environmental Implications
• Xe isotopic constraints on cycling of deep Earth volatiles
• Apollo's Agglutinates: An Analysis of Lunar Agglutinate Reflectance and Implications for Space Weathering
• Broadband seismic response of the Ross Ice Shelf to tidal forcing observed by stations near grounded ice margins
• Determining Regolith Production Rates and Landing Site Safety Hazards Using Boulder Distributions Around Small, Young Lunar Impact Craters
• Developing a Streamlined Field Protocol for In Situ Sequencing and Analysis of Extremophiles
• Effects of heat-producing elements on the long-term evolution of thermochemical piles at the base of the mantle
• International Planetary Data Alliance: Current and Future Plans
• Investigating Local Variations of Lunar Rock Types at Sites of "Purest Anorthosite" Detection
• Microseismicity along Major Ross Ice Shelf Rift Resulting from Tidal Stresses and Thermal Contraction of the Near-Surface Firn Layer
• Overview of Recent Results from Opportunity's Investigation of Endeavour Crater and Perseverance Valley
• P Wave Velocity of the Upper Mantle in the Region of Tatar Strait: Constraints from Triplicated Waveforms
• Seismicity of the Incoming Plate and Forearc at the Mariana Trench Recorded by Ocean Bottom Seismographs
• The Role of the Next Generation Lunar Scientists and Engineers (NextGen) Group in Lunar Science and Exploration
• Variations in Local Geology and Regolith Properties at Apollo 17: Correlating Photometric Analyses with Soil Composition and Physical Characteristics
• Xe Isotopic Constraints on the History of Deep Earth Volatile Recycling
• AGU Celebrates its Centennial with the Initiation of a New Journal: Perspectives in Earth and Space Science
• An isotopic journey through space and time: exploring the connections between atmospheric circulation, local hydrology, and precipitation isotope ratios in paleo-monsoons using an isotope-enable general circulation model.
• An updated dust aerosol model for Mars
• Boron isotopic constraints on slab and mantle-derived fluid and melt sources of Nicaraguan volcanics
• Constraints on the lithospheric structure of southern Patagonia from receiver function and surface wave analysis
• Crystal exit interviews - the role of olivine in recording magma assembly and magmatic processes
• Decoding Cenozoic Tectonics in Patagonia, the Scotia Sea, and the Antarctic Peninsula from New Seismic Tomography
• Deep Learning Using a Convolutional Neural Network for the Classification of Seismic Green's Functions
• Defining 'pre-industrial climate': Past global changes during the most recent two millennia
• Evaluation of triple oxygen isotopes in daily East African precipitation as a potential tracer of recycled continental moisture
• Evidence of correlation between surface winds and methane abundance in Gale Crater, Mars
• Helium and carbon isotopes in southern Costa Rica and western Panama
• In-situ investigation of periodic bedrock ridges in the Glen Torridon area with the MSL Curiosity rover, Gale crater, Mars
• Intrepid: Lunar Roving Prospector
• Investigation of climate, terrestrial ecosystems, and aquatic productivity during the past 1,500 years from the Lake Sibinacocha watershed, Peruvian Andes
• Measuring actinide partitioning in zircon to improve the <SUP>230</SUP>Th correction for <SUP>206</SUP>Pb/<SUP>238</SUP>U dates
• New insights into spatial and temporal dynamics of the global water cycle from the Iso2k database
• Potassium Isotopic Composition of Loess
• Reconstructing landscape scale vegetation in tropical Central America using bat guano carbon isotopes
• Seismic Imaging of the Mariana Subduction Zone: An Overview
• Superimposed Signatures of Ancient Heterogeneity and Long-term Volatile Transport from Noble Gases
• The History, Challenges, and Achievements of Passive Broadband Seismic Investigations in Antarctica
• The Interdisciplinary Consortium for Evaluating Volatile Origins (ICE Five-O)
• The Limits of Glassy Melt Inclusion as Magmatic H<SUB>2</SUB>O Recorders for Super-Hydrous Mafic Melts
• The PAGES 2k Network: Overview, Progress and Vision
• Topography of the 410-Discontinuity in Subduction Zone from Nonlinear Inversion of Triplicated Waveforms
• What record will the Greenheugh pediment and associated landforms in Gale crater reveal about Martian climate history?
• δ<SUP>13</SUP>C and δ<SUP>2</SUP>H of Amino Acids in Escherichia coli (E. coli) Altered by Catabolic Enzyme Knockouts
• A Unique Sodic Mafic Igneous Achondrite From an Ancient(?) Differentiated Parent Body
• Adapting the Compact Integrated Raman Spectrometer(CIRS) for the Europa Lander Mission Concept
• Advancing community-led research into the climate of the Common Era
• Along Strike Variations in Structure and Melt Production in the Lau Back Arc Spreading Center from Body-wave Tomography
• Antarctic Network - Polar Earth Observing Network: Achievements from Ten Years of Autonomous Measurements
• Apollo Next Generation Sample Analysis: What to expect among Rock Fragments in Apollo 17 Core Samples 73001 and 73002
• Assessment of 19<SUP>th</SUP> and 20<SUP>th</SUP> century lake and air temperature history in the Peruvian high Andes using biomarkers and lake energy balance modeling
• Chloramphibole in Nakhlite Northwest Africa 13368 and Implications for Halogens on Mars
• Coherent, Millennial-Scale Trends in δ<SUP>18</SUP>O: A Fingerprint of Pacific Walker Circulation Changes?
• Experimentally Testing Whether Magmatic Processes can Produce Strong Lunar Crustal Magnetism
• Fingerprinting the Pacific Walker Circulation Using Precipitation δ<SUP>18</SUP>O
• Hematite-Bearing Materials on Mars Identified and Characterized Using MRO CRISM, Opportunity, and Curiosity Data
• High Spatial Resolution Thermal Inertia Mapping of Mount Sharp and Northern Plains, Gale Crater, Mars
• Higher education teaching resources on imperialism and scientific racism in the geosciences, from past to present
• How I Use Changes in the Number of Tiny Things in a Piece of Water to Guess How a Big Air Circle Changed in the Past
• Identification and Characterizations of the Basal Sulfate-Bearing Stratum, Northern Mount Sharp, Mars
• Intrepid: Traversing 4 Billion Years of Lunar History
• Lunar Agglutinate Glass Composition and Implications for Agglutinate Formation
• Mantle plume source volatile accretion, degassing and regassing
• Modeling memory in gravel bed rivers: consideration of a discharge-dependent threshold for motion
• New evidence for climate and erosion history in Gale crater, Mars, from Curiosity's ascent onto the Greenheugh pediment
• Petrology of soils from the landslide deposit at Taurus-Littrow: Context for the ANGSA double drive tube 73001/73002 from Apollo 17
• Phylogenetic, Adaptational, and Environmental Controls on Hydrogen Isotope Apparent Fractionation in Leaf Waxes from a Synthesis of 3,000+ Plant Specimens
• Probing coupled processes in the laboratory from pore scale to whole core scale
• Science Targets in the Analyst's Notebook: Addition of MER Contact Science Targets and New Functions for MSL and MER
• Sulaimaniyah 2015 Earthquake Swarm Analysis Using Matrix Profile TechniqueI
• The Role of Paleoecology in Elucidating the Spatiotemporal Dynamics of Tundra Fires
• The unusual 2018-2019 rainy seasons in western Uganda through the lens of precipitation isotopes, satellite data, and farmer observations
• Upper Mantle Seismic Anisotropy of Antarctica from Shear Wave Splitting Analysis
• Using LROC NAC Photometry to Study the Moon's Feldspathic Crust
• Windblown Basaltic Sands on the Northern Slopes of Mount Sharp and Adjacent Plains, Gale Crater, Mars

Linked Collaborating Authors [?]

• Alessandro Frigeri
• E. Heggy
• G. Bellucci
• J. D. Stopar
• Laura Schaefer
• R. E. Arvidson
• R. Noschese
• R. Orosei
• S. Erard
• Thomas M. Mitchell