Carnegie Institution of Washington, Geophysical Laboratory

    flowchart
    I[Carnegie Institution of Washington, Geophysical Laboratory]
    PI["Parent Institutions (1)"]
    CI["Child Institutions (0)"]
    AW["Affiliated Works (641)"]
    CA["Linked Collaborating Authors (14)"]
    I== skos:broader ==>PI
    CI== skos:broader ==>I
    AW== affil ==>I
    AW== author ==>CA
    click PI "#parent-institutions"
    click CI "#child-institutions"
    click AW "#affiliated-works"
    click CA "#collaborating-authors"

ADS ID [?]

A00147

Abbreviation [?]

Geop Lab

Parent Institutions [?]

• Carnegie Institution of Washington

Child Institutions [?]

Affiliated Works

sorted by decreasing year, and then by display-name

• Diamond anvil cell investigation of lattice strains and preferred orientation in iron at high pressure and temperature.
• Diffusion of magnesium and oxygen in MgO at lower mantle conditions
• Experimental Mineralogy and the Origin of Life
• Experimental study on the lattice dynamics of iron at high pressures and high temperatures
• Generation of Mid-ocean Ridge Basalts at Pressures From 1 to 7 GPa
• In Situ X-ray Diffraction Measurements of the Postspinel Transition in Mg<SUB>2</SUB>SiO<SUB>4</SUB>
• Influence of magnetism on spectroscopic and elastic properties of hcp iron
• Inner core elasticity and temperature from first principles
• Oxygen Isotopes and the Cooling History of the Mount Barcroft Area, Central White Mountains, Easternmost California
• Phase Relations in the System Mg<SUB>2</SUB>SiO<SUB>4</SUB>- MgAl<SUB>2</SUB>O<SUB>4</SUB> at 22 GPa
• Potassium Partitioning Between Iron Sulfide and Peridotite Melt at 2.0 GPa
• Structure and Bonding in Transition Metal Sulfides: Merging Experiment and Theory
• Temperature Distribution in Multi-Anvil Assemblies Derived From Spinel Layer Growth
• Temperature and Compositional Dependence of Hydroxyl Solubility in Coesite
• The CaCl<SUB>2</SUB> transition in Stishovite
• The diamond anvil cell as a deformation apparatus for investigating the rheology of the deep Earth
• X-ray Diffraction and Raman Spectroscopy of SrGeO<SUB>3</SUB> at High Pressure
• X-ray Spectroscopy at Ultra-High Pressure: Present and Future
• Advancing in the Extremes of Pressure and Temperature: New Generation of Experimental Studies of Earth and Planetary Interiors
• Biomarkers: d13C and d15N Distribution Tightly Coupled to Nutrient Dynamics and Viral Lysing in a Microbial Mat From Death Valley, California
• Catastrophic Ecosystem Collapse in Pleistocene Australia
• Constraining the equation of state of fluid H<SUB>2</SUB>O to 60 GPa using the melting curve of Ice VII and the formation of Mg(OH)<SUB>2</SUB> in the MgO-H<SUB>2</SUB>O system.
• Constraints on the Composition of the Outer Core From the Equations of State and Other Properties of Liquid Fe,S,Si-alloys.
• Crystal chemistry and mineral physics of silicate perovskite in the Earth's lower mantle
• Deformation of silicate perovskite aggregates up to 30 GPa
• Diamond-Anvil Cell Research Facility at the X17B Beamline of National Synchrotron Light Source
• Diffusion of Siderophile Elements in Fe-Ni Alloys at High Temperature and 10GPa
• Direct Observations Of Microbial Activity At Extreme Pressures
• Elasticity of Antiferromagnetic hcp Iron
• Eleven Years of CHiPR [1991-2002] and Its Legacy
• High Pressure Structural Properties of FeAlO<SUB>3</SUB>
• High-Pressure Hydrothermal Processing in Large Icy Satellites
• High-pressure Polybaric Fractionation and Spinel-Garnet-Liquid Reactions in Garnet-bearing Xenoliths from Oahu: Evidence from CMAS
• Hydrogen Storage in Clathrate Hydrate
• In-situ Single-Crystal Neutron Diffraction on Hydrogen Related High-Pressure Compounds at High-Pressure
• Iron-Nickel Phosphides at High Pressures and Temperatures
• Large S-33 Anomalies in Late Archean Carbonacous Shales
• Layer Shift Phase Transitions in the Kaolin Polytypes
• MIF in Archean Rocks: An Evidence of S8 Aerosols in the Archean Atmosphere?
• Magnesiowüstite (Mg<SUB>0.64</SUB>Fe<SUB>0.36</SUB>)O Thermal Equation of State to 25 GPa and 2073 K
• Mid-Infrared Radiation, Electric Charges, and Acoustic Emission During Rock Deformation
• Neutron Diffraction Study of Silicate Perovskites
• New results on H<SUB>2</SUB>O Ice VI. Phase equilibria, elasticity, molecular geometry and proton disorder.
• Osmium Isotopes from Appalachian Ophiolite Chromites
• Phonon Density of States and Elasticity of Iron-Based Materials at High Pressures
• Synchrotron infrared spectroscopy of OH-chondrodite and OH-clinohumite at high pressure
• The Minimum Potential Temperature of the Hawaiian Mantle is About 1420°C
• The Nature of Polymerization in Silicate Glasses and Melts: Solid State NMR, Modeling and Qauntum Chemicial Calculations.
• The Seismogenic Properties of Subducted and Unsubducted Oceanic Lithosphere
• X17C - The Superconducting Wiggler Beamline Dedicated for Diamond Cell Research
• A Radioactive Heat Source in Planetary Cores: Experimental Evidence for Potassium
• Atomistic Simulations of PbTiO<SUB>3</SUB>, PMN, and PMN-PT: using shell model potentials fitted to first principles results
• Chemical Order in Silicate Melts: Implications for Microscopic Origins of Mantle Melting Behavior
• Comparison of gold and MgO pressure scales at 22-56 GPa and 300-1150 K and its implications for mantle models
• Electronic spin state of iron in lower mantle perovskite
• Equation of State of (Mg<SUB>0.92</SUB>, Fe<SUB>0.08</SUB>)SiO<SUB>3</SUB> Perovskite from Shock Wave Study and its Geophysical Implications
• Estimating peak last-interglacial warmth in the Eastern Canadian Arctic
• Examination of an Oligocene Lacustrine Ecosystem Using C and N Stable Isotopes
• Extension of (Mg<SUB>0.64</SUB>Fe<SUB>0.36</SUB>)O Ferropericlase Equation of State Measurements to 25 GPa and 2173 K
• Finite-temperature Properties of bcc Fe
• Frontiers of High-Pressure Research: Next Generation Large Volume Gem Anvil Devices
• Frontiers of High-Pressure Research: Synchrotron Infrared Spectroscopy
• High Pressure Elasticity of Iron Alloys From Nuclear Resonant Inelastic X-ray Scattering and X-ray Diffraction
• High-pressure and High-temperature Studies With Nuclear Resonant Scattering
• In Situ High P-T Raman Spectroscopy and Laser Heating: Applications to Volatiles Under Deep Earth Conditions
• In Situ High Pressure Angle Dispersive X-ray Diffraction Experiments:With Sagittally-Bent Double Laue Monochomator
• In Situ Observation of Anisotropy Development With Pressure to 50 GPa in Olivine, Ringwoodite, Magnesiowuestite and Silicate Perovskite
• Layer shift phase transition in kaolins by computer
• Magnetic and structural transition in Fe<SUB>3</SUB>S at high pressures
• Microstructural Study of Synthetic Sintered Diamond and Comparison with Carbonado, a Natural Polycrystalline Diamond
• Monitoring the Evolution of Electronic Band Gaps in Simple Molecules at High Temperature and Pressure
• Neighborite Under High Pressure: In Situ Angle Dispersive X-ray Diffraction Study Using Synchrotron Radiation
• New Non-local Density Functionals for More Accurate First-principles Calculations
• Nuclear Magnetic Resonance Spectroscopy in the Diamond Anvil Cell
• Ocean Island Lavas: Garnet Clinopyroxenite or CO2-bearing Mantle Lherzolite?
• Origin and Evolution of Mantle Lithosphere
• P-V-T Equation of State of Al-bearing Silicate Perovskite and its Implications for Mantle Composition Models
• P-V-T equation of state of ɛ -FeSi
• Phase Transformation of Al<SUB>2</SUB>O<SUB>3</SUB> Under High Pressure and High Temperature and its Effect on Ruby Pressure Scale
• Role of Impact-Induced, Vapor-Phase Deposition in the Lunar Regolith Formation: Clues from the New Mineral, Hapkeite
• Stability and P-V-T Equations of State of High-Pressure Iron-Sulfur Compounds
• Stability of Perovskite under Lower Mantle Pressure and Temperature Conditions
• Stable Isotope Analyses of Phosphate Oxygen From Micro-samples of Biological Apatite: A new Routine Procedure for Silverphosphate Micro-precipitation and the Removal of Organic Contamination
• Structures and Properties of Silicate Glasses and Melts at High Pressure: Multi-nuclear 2 Dimensional Solid State NMR and Statistical Mechanical Modeling
• Study of Sound Velocities of Iron With Nuclear Resonant Inelastic X-ray Scattering Under High Pressure and Temperature
• The Effect of Pressure on Diffusion of Au, Pd, and Re in Fe-Ni Alloys
• The Future of Computational Mineral Physics
• The Implications of Different Geotherms for the Generation of Carbonatites, Kimberlites and Melilitites
• Tracking Urban Air Deterioration in San Francisco: Carbon and Nitrogen Isotope Study of Weedy Plants.
• Ultrasonic Shear Waves in the Diamond-Anvil Cell and Shear-Mode Softening in (Mg,Fe)O
• Upper Mantle Seismic Velocity Structure beneath East Africa and the Arabian Peninsula
• X-Ray Microdiffraction at Megabar Pressures
• A Primitive Achondrite With Oxygen Isotopic Affinities to CV Chondrites: Implications for Differentiation and Size of the CV Parent Body
• Crystal Chemistry of Transition Metal Arsenides and the High Pressure Behavior of CoAs
• Deformation Experiments at High Pressures in Diamond Anvil Cells: Texture Development in MgSiO3 Perovskite
• Deformation of polycrystalline Ca-Perovskite up to 50 GPa
• Dependence of Water Solubility in Mantle Olivine on the Silica Activity
• Elastic Properties of Zinc Ferrite and Aluminate Spinels
• Elastic Versus Non-Elastic Co-Seismic Strain Response at the Trizonia Borehole Sacks Evertson Dilatometer in the Rift of Corinth, Greece, for a Local, Moderate Earthquake.
• Elasticity and stability of FeSi at high pressures
• Experimental Partitioning of U Between Liquid Iron Sulfide and Liquid Silicate: Implications for Radioactivity in the Core
• Experimental constraints on silicon in the Earth's core
• Ferromagnesian Post-Perovskite Silicates in the D" Conditions
• Generation of Methane Via High Pressure Carbonate Reduction
• Generation of Primary Kilauea Magmas: Constraints on Pressure, Temperature and Composition of Melts
• High Pressure IR And XRD Studies For Hydrous Minerals
• High pressure NMR spectroscopy of clathrate hydrates
• High-pressure elasticity of Fo90 hydrous ringwoodite
• Hot Hawaii, Cold Ridges, Mantle Heterogeneity, and Plumes
• Hydrous Synthesis of Aluminum Bearing Silicate Perovskite: Implications for Hydrogen Storage in the Lower Mantle
• In situ X-ray diffraction and X-ray emission study of magnesiowustite in Earth's lower mantle conditions: implications to the geophysics and geochemistry of the lower mantle
• Investigation on cell assemblies for mantle rheology
• Length-Scales of Oxygen, Hydrogen, and Argon Isotope Exchange During UHP Metamorphism: an Example From the Qinglongshan UHP Eclogites (Sulu Terrain, China)
• Liquidus Phase Relations in Pyrolite at Pressures of the Transition Zone
• Minor and Trace Element Partitioning Among α -, β - and γ -(Mg,Fe)<SUB>2</SUB>SiO<SUB>4</SUB> in Fertile Peridotite KLB-1: a High Pressure Experimental Study
• Na- and Zn- bearing (Mg,Fe)Al2O4 spinel exsolution from ilmenite and magnetite of eclogite in the CCSD Main Hole
• Nuclear Resonant Scattering Studies Under High Pressure and HighTtemperature
• P-V-T equations of state of lower mantle minerals: Constraints on mantle composition models
• Path Integral Simulations of Hydrogen Melting at High Pressures
• Phase stability of CaSiO<SUB>3</SUB> perovskite at high pressure
• Post-Perovskite Phase in Al<SUB>2</SUB>O<SUB>3</SUB> and Implications for the Lower Mantle
• Potassium as a Radioactive Heat Source in the Core? A High Pressure Experimental Study
• Second Critical Endpoint in Peridotite-H2O System and its Bearing on the Magmatism in Subduction Zones
• Study of sound velocities of hcp-Fe with nuclear resonant inelastic x-ray scattering in a laser-heated diamond cell
• Teaching optical mineralogy as a skill for mineral physics
• The Oxygen Isotope Composition of Earth and the Terrestrial Fractionation Line (TFL)
• Trace Element Partitioning Between Metal and Melt at High Pressure
• Understanding the Mechanism of Deep Earthquakes: A new System for Detecting Acoustic Emissions in Multianvil Experiments
• Valence state of iron in mantle phases at high pressures and high temperatures
• δ <SUP>13</SUP>C and δ <SUP>15</SUP>N Values of Soil Organic Matter Over Drought and Non-drought Affected Elevation Gradients in Ethiopia: Calibrating for Environmental Reconstruction
• Acoustic wave propagation at a cobalt/helium interface - high pressure elasticity of hexagonal metals.
• Aggregate Elastic Moduli and Equation of State of B2 Phase of NaCl to 73 GPa by Simultaneous Synchrotron X-ray Diffraction and Brillouin Scattering Measurements.
• Atomistic and Nanoscale Origins of Macroscopic Properties of Silicate Melts at High-Pressure: Spectroscopy &amp; Quantum Chemical Calculations
• Chemistry of Xenon With Earth's Materials.
• Chemolithoautotrophy and its Relation to Magnetism and Biomineralization in Marine Magnetotactic Bacteria
• Comparison of Quantum and Classical Monte Carlo on a Simple Model Phase Transition
• Constraining Rates of Biodegradation of Chlorinated Ethenes at Steep Concentration Gradients Using Stable Carbon Isotopes
• Detecting Acoustic Emissions With/Without Dehydration of Serpentine Outside P-T Field of Conventional Brittle Failure
• Effect of chemistry on the physical properties of perovskite and post-perovskite (Mg,Fe,Al)(Al,Si)O3
• Effects of the Spin Transition of Iron in Magnesiowuestite
• Effects of water on the behavior of MgSiO3-clinoenstatite at high pressure
• Elastic moduli and equation of state of NaCl to 30 GPa by simultaneous x-ray density and Brillouin sound velocity measurements
• Elastic properties of dense oxide minerals and other applications of GHz-ultrasonic interferometry
• Element partitioning during core-mantle differentiation in a magma ocean: New high-pressure data on CI- and EH-chondrite model compositions
• First-principles thermoelasticity of hexagonal-close-packed iron at high pressures
• Garnet-melt partitioning at 10 GPa in the CMAS-CO2 system: a link between CO2-rich melts and majoritic-garnets in diamonds from the mantle?
• H2O under Extreme Conditions
• High-Temperature Fractionation of Iron Isotopes During Metal Segregation From a Silicate Melt: Experimental Study of Kinetic and Equilibrium Fractionation
• High-pressure elasticity of perovskite and post-perovskite (Mg,Fe,Al)(Al,Si)O3
• High-pressure synchrotron-IR studies of hydrous transition zone and lower-mantle minerals in the laser-heated diamond cell
• High-pressure vibrational study of dense hydrous magnesium silicate 10A Phase
• Hydrogen Solubility in Al-bearing Perovskite
• In-situ Sound Velocity Measurements on bcc and hcp Phases of Fe
• Integrated in-situ probes for structural and dynamic properties of geological materials at ultrahigh pressures and temperatures
• Magmatic Ultramafic Rock in Sulu Ultrahigh Pressure Metamorphic Belt: Depleted Oxygen isotope Evidence From Main Hole of Chinese Continental Scientific Drilling Project
• Majoritic garnet-silicate melt partitioning of trace elements between 10 and 17 GPa in an anhydrous fertile mantle composition
• Na8-Fe8-Depth Systematics of MORBs: Implications for Melting Models, Temperature, and Mantle Heterogeneity
• New Experimental Setup for High-Pressure High-Temperature Gigahertz Ultrasonic Interferometry
• Physics and chemistry of ferromagnesian silicate post perovskite
• Plastic deformation of MgGeO3 post-perovskite beyond 100 GPa
• Second critical endpoint in the basalt-H2O system
• SiO2 Solubility in Rutile at High Pressure and Temperature
• Spin Transition in (Mg,Fe)O at High Pressure
• Stable Isotopes, Multidisciplinary Studies, and the Leadership of J.G. Liou in UHP Metamorphism
• Structural refinement for NaMgF3 perovskite under high pressure
• Structure and Transport Properties of Hydrogen Filled Ices (H2O:1/6H2 and H2O:H2) at Pressures to 4 GPa by Solid State Diamond-Anvil-Cell NMR
• The Effect of Composition on Diffusion of Au in Fe and Fe-Ni Alloys
• The Experimental Degradation of Microorganisms Exposed to Mn(II) and SiO2 Over Time
• The Heterogeneous Hawaiian Lithosphere: New Isotope Data From Kauai and Oahu Peridotites
• Unique Angrite NWA 2999: The Case For Samples From Mercury
• A Chemical Comparison of STARDUST Organics with Insoluble Organic Matter in Chondritic Meteorites
• A Fresh Plutonic Igneous Angrite Containing Grain Boundary Glass From Tamassint, Northwest Africa
• An Experimental Investigation of Melting Relations in the Fe-C System at High Pressure and Temperature
• Anomalously low pressure of rutile-CaCl2 phase transition in aluminous hydrogen- bearing stishovite.
• Biogeochemical Carbon Cycling in Ultrabasic Reducing Springs in Sonoma County, CA
• Challenges to Determining Metal-Silicate Element Partition Coefficients Under Extreme P-T Conditions
• Conduction in the Lower Mantle: Optical Absorption Spectra of Iron-Bearing Magnesium Silicate Perovskite at Lower Mantle Pressures
• Detection of Cellulose and Comparative Biopolymeric Analyses of low pH, Sub-aerial Biofilms of the Richmond Mine, Iron Mountain California
• Direct Shock Loading of Pre-synthesized MgSiO3-perovskite Sample to the Earth`s Lower Mantle Conditions and Its Geophysical Implications
• Dissolved Carbon Species in Diffuse and Focused Flow Hydrothermal Vents at the Main Endeavour Field, Northern Juan de Fuca Ridge
• Dynamic mean-field theory study of FeO
• Effect of the FCC to HCP Phase Transition on Trace Element Partitioning Between Metal and Sulfide Melt
• Elasticity of iron-rich silicate in Earth's D" layer
• Evidence for a Carbonaceous Chondrite Parent Body With Near-TFL Oxygen Isotopes From Unique Metachondrite Northwest Africa 2788
• Experimental Abiogenic Synthesis and Stable Carbon and Hydrogen Isotope Values of Gaseous Hydrocarbons and the Implications for Identifying Biosignatures
• Experimental determination of elasticity of iron at high pressure
• High Pressure Calibration at High Temperatures in the Diamond Anvil Cell Using Cubic Boron Nitride
• High Pressure Infrared Spectra of Talc and Lawsonite
• High-Pressure High-Temperature Raman Spectroscopy of San Carlos Olivine
• In-situ X-ray Diffraction Measurements of Ferropericlase up to 110 GPa and 2000 K
• Microbially Induced Sedimentary Structures Biosignatures Rising From Biotic-Physical Interaction in Siliciclastic Tidal Flats
• Microscopic Origins of Configurational Thermodynamic Properties of Silicate Melts at Ambient and High Pressure
• Multiscale Modeling of Iron at high temperatures and pressures
• NaCl and Neon as Pressure Standards and Media
• Neutron and x-ray scattering studies for Fe1-xO
• Oscillation Laue Analysis (OLA) - A new crystal structure determination method for mineral physics
• Polycrystalline and Intracrystalline Growth of Akimotoite in Clinoenstatite of the L-6 Tenham Chondrite
• Quantum Monte Carlo Simulations of Phase Transitions in Silica
• Raman and infrared spectra of stibnite, Sb2S3
• Redox and pH Evolution of the Subseafloor Hydrothermal System at the Main Endeavour Field, JDF: Constraints From Time Series Measurement Using In-Situ Chemical Sensors
• Self Consistent Equation of State for Dense Argon
• Simulations of Silica Phases Beyond the Generalized-Gradient Approximation
• Sound Velocities and Spin States of Magnesiowustite in the Earth's Lower Mantle
• Sound Velocities at the Spin Crossover in (Mg0.75Fe0.25)O Ferropericlase
• Sound Velocities for Ferrous Periclase Through the High Spin - Low Spin Transition
• Sound velocity of MgSiO3 post-perovskite phase: Constraints on the D" discontinuity
• Structure of Oxide Glass and Melts at High-Pressure: A View from Inelastic X-ray Scattering and 2D Solid-State NMR
• Synchrotron x-ray scattering studies for minerals under high pressure
• Synthesis and high-pressure synchrotron-infrared studies of OH-bearing silicate perovskite in the laser-heated diamond cell
• The effect of minor elements on H incorporation in MgSiO3 perovskite
• Theoretical and Experimental Raman Study of Spinel
• Thermal densification of GeO2 glass under high pressure
• Ultrabasic Spring Geomicrobiology of the Cedars Peridotite
• Viscosity of liquid iron derived from the liquid structure data at high pressures
• Assessing the Habitability and the Biogeochemical Output of Subsurface Biomes
• Biogeochemistry and nitrogen cycling in an Arctic, volcanic ecosystem
• CO2 Laser Heating System at GSECARS
• Compressibility and phase transition studies for amorphous materials under high pressure: Approach combined of synchrotron high energy x-ray diffraction and micro tomography techniques using diamond anvil cell
• Effect of alloying elements on the magnetic transitions in iron-rich alloys
• Field Study of Mars Analog Materials in Spitsbergen (Norway) Using a Portable X-ray Diffraction Instrument
• High-Accuracy Pressure Scale Computed With Quantum Monte Carlo
• High-Pressure Raman Spectroscopy of Protonic Diffusion in ice VII
• Material Yield Strength and Anisotropy in the Nonhydrostatic Diamond Anvil Cell: Implications for Mantle and Core Minerals
• Melting behavior of (Mg,Fe)O solid solutions at high pressure
• New Constraints on the Pyrolitic Model: In Situ X-ray Diffraction Measurements on KLB-1 Peridotite Under the Lower Mantle Conditions
• New Experimental Method for In Situ Determination of Material Textures at Simultaneous High-Pressure and -Temperature by Means of Radial Diffraction in the Diamond Anvil Cell.
• Phase relations of iron determined by in-situ x-ray diffraction in an internally-heated diamond anvil cell
• Pressure-Induced Changes in Crystal-Melt Partitiong Coefficient between Silicate Melts and Crystals: A View from Solid-State NMR
• Pressure-Induced Phase Transitions In Gadolinium Iron Borate
• Progress in Life Marker Chip Technology for Detection of Life on Mars
• Quantum Monte Carlo Computations for Equations of State, Phase Transitions, and Elasticity of Silica
• Quantum Monte Carlo Study of the Elastic Instability of Stishovite Under Pressure
• Reduced Seismic Anomalies in the Lower Mantle: Role of the High-Spin to Low-Spin Electronic Transition
• Simple Molecular Systems Under Simultaneous Conditions of High Pressure and Temperature
• Spin Transition Zone (STZ) in the Lower Mantle
• Spin Transition and Equation of State of Ferropericlase at High Temperature: Implications for Density Model of the Lower Mantle
• Structure and Properties of Amorphous MgSiO3 in Earth's Mantle: A View from Synchrotron Inelastic X-ray Scattering
• Subduction of Continental Crust into Earth's Transition Zone: an Experimental Investigation with Implications for the Fate of Continental Subduction
• Sugar-Mineral Interactions and the Origins of Life
• Synchrotron Infrared Reflectivity of Iron at High Pressure
• Synchrotron x-ray diffraction studies for zincite and ceria under high pressure conditions
• The Electronic Structure of Iron in (Mg,Fe)SiO3 Perovskite and Post-Perovskite Under Megabar Pressures
• The High Pressure Synergetic Center at the Advanced Photon Source
• The equation of state and structure stability of elemental metal vanadium under high pressure -from experiments to theories
• Toward a self-consistent pressure scale: elastic moduli and equation of state of MgO by simultaneous x-ray density and Brillouin sound velocity measurements at high-pressure high-temperature conditions
• Towards Determining the Upper Temperature Limit to Life
• Water at the Bottom of Upper Mantle: A Key to Reconcile Mineral Physics Composition Model with Seismic Wave Velocity Jump at 410-km Discontinuity
• X-ray induced dissociation of H2O and formation of an O2- H2 compound at high pressure
• Adsorption of Aspartic Acid onto Rutile: Implications for Biochirality
• An Archean Terrestrial Fractionation Line for Oxygen Isotopes
• Atomistic Origins of Densification in Oxide Melts in Earth's Mantle: Insights from Synchrotron X-ray Raman Scattering
• Clathrates from Carbonates: New In-Situ Observations of Carbonate-Derived Methane at Mantle Pressures
• Deformation of MgSiO3 perovskite at high pressure using diamond anvil cells and in- situ radial diffraction
• Detailed structure of the carbonated peridotite solidus ledge in the system CaO-MgO- Al2O3-SiO2-CO2
• Distinguishing Multiple Surface Species of Glutamate on Hydrous Ferric Oxide (HFO)
• Do Secular Trends in the Nickel Content of Banded Iron Formation Record a Methanogen Famine?
• Effect of Water on topography of 660 km Seismic Discontinuity: Experimental View
• Experimental Survey of Microbial Survival at High Pressure
• Geochemical and Biochemical Co-Evolution of Uranium and Thorium Minerals
• HCP vs. FCC vs. BCC iron phases in the Earth' s inner core
• High Temperature Theory of Iron and Iron-Nickel from Surface to Core
• High-pressure behavior of iron-nickel-cobalt phosphides and its implications for meteorites and planetary cores
• High-pressure single-crystal X-ray diffraction study on Super Fluorous Phase B up to 7.4 GPa
• In Situ Determination of BCC-, FCC- and HPC-Iron Textures at Simultaneous High- Pressure and -Temperature by Means of the Resistive Heated Radial Diffraction Diamond Anvil Cell (RH-RD-DAC): Implications for the iron core.
• In Situ Thermal Diffusivity Measurements Of MgSiO3 Perovskite At Lower Mantle Pressures
• Infrared Spectroscopic Evidence of Surface Speciation of Amino Acids on Titanium Dioxide
• Kinetic Studies of Amino Acid Adsorption on Rutile
• Kinetics of H2-O2 Redox Equilibria and Metastable Formation of H2O2 Under low Temperature Hydrothermal Conditions
• Magnetism in Metal Oxides Under Pressure
• Melting at High Pressures
• Melting in the system CaO-MgO-Al2O3-SiO2-FeO-Cr2O3 spanning the plagioclase-spinel lherzolite transition at 7 to 10 kbar: experiments versus thermodynamics
• Mixed Spin State of Iron in a New Post-Perovskite Silicate at Earth's Core-Mantle Boundary
• MoS2 and ReS2 Stabilities as Indicators of the Oxidation State on the Early Earth
• NanoSIMS Analysis of Sulfur Isotopes in Sulfides from ca. 2.7 Ga BIFs and Cherts as Tracers of Microbial Activity
• On the Evolution of Mineral Biosignatures
• P-V-T Equation of State of (Al,Fe)-bearing Mantle Perovskite and its Implications for Mantle Models
• Partitioning Behavior of Oxygen Between Fe-S Alloy and Silicate
• Phase relations in the peridotite-carbonate-chloride system at 7.0-16.5 GPa and the role of chlorides in mantle dynamics
• Predominant Intermediate-Spin Ferrous Iron in Lowermost Mantle Post-Perovskite and Perovskite
• Preferential Treatment: Interaction Between Amino Acids and Minerals
• Probing and Modeling of Pressure-induced Structural Transformation in Oxide Melts at High Pressure
• Producing Martian Lithologies with Geophysically-Constrained Martian Mantle Compositions
• Quantum Monte Carlo Computations for Minerals at High Pressures
• Redetermination of Post-Perovskite Structure of (Mg,Fe)SiO3
• Searching for the Origins of Extraterrestrial Matter
• Spin Crossover and Thermal Conductivity in the Earth's Lower Mantle
• Spin state and valence state of iron in Earth's lower mantle from synchrotron Mössbauer spectra of perovskite and post-perovskite up to 1.5 Mbar
• Structure and Compressibility of Iron- and Aluminum-bearing Phase D
• Structure of interatomic Fe-B compounds at high pressures and temperatures
• The Oxygen Isotope Composition of PO4 Extracted From Lost City Hydrothermal Vents -- a Potential Biosignature for Vent Hosted Microbial Ecosystems
• The behavior of iron in (Mg,Fe)SiO3 post-perovskite at megabar pressures
• Tracing the origin of carbonaceous matter and apatite in Neoarchean banded iron formations from Abitibi
• Water-rich carbonatites at low pressures and kimberlites at high pressures
• 2009 Arctic Mars Analogue Svalbard Expedition (AMASE) Evolved Gas Studies
• A link between Interstellar Formaldehyde and Chondritic and Cometary Organic Solids
• Advances in understanding of electronic transitions in FeO under compression
• Astrobiology, Evolution, and Society: Public Engagement Insights
• Clumped-isotope thermometry of speleothems: understanding and correcting for large kinetic fractionation induced by CO2 degassing
• Comparison of the Organic Composition of Cometary Samples with Residues Formed from the UV Irradiation of Astrophysical Ice Analogs
• Constraints on the Nature of Hydrothermal Magmatic Fluids that can produce Sulfate-rich Alteration Assemblages on Mars
• Crossover from Melting to Dissociation in Carbon Dioxide at 35 GPa
• Direct density measurements under mantle and core conditions and chemical characterization of high-PT samples (Invited)
• Effect of silicon on the equation of state and crystal chemistry of hcp iron up to 150 GPa and 2500 K
• Evolution of uranium and thorium minerals
• Fenton Oxidation of H2O2 under Low Temperature Hydrothermal Conditions: Implications for Organics on Mars
• Fractionation of Sulfur Isotopes in the Formation of Mars
• High-Precision Stable Isotope Analyses with the NanoSIMS 50L (Invited)
• Hydrogen solubility in omphacite up to 10 GPa and implications for water transportation in subduction zone
• Hydrous Ringwoodite: Clarifying Defect Mechanisms Through Combined Single-Crystal Refinement, Compressibility, and IR Spectroscopy
• Improving EPMA Standards and Standards Measurement by Updating Correction Parameters, Refining Measurement Procedures, and Accounting for Surface Coatings (Invited)
• In situ high-pressure single-crystal X-ray diffraction study of chromite
• Interactions between glycine derivatives and mineral surfaces: Implications for the origins of life on planetary surfaces
• Isotopically Anomalous Carbonaceous Nanoglobules in Meteorites and Comets
• Measurement of thermal conductivity of Mg0.9Fe0.1SiO3 perovskite at high pressure and temperature
• Mechanisms for “Vital Effects” in Biogenic Carbonates: New Perspectives Based on Abundances of 13C-18O Bonds
• Molecular Insights into Plant-Microbial Processes and Carbon Storage in Mangrove Ecosystems
• Multiple Accelerating Potential SEM Microanalysis of Individual Atmospheric Particles (Invited)
• Nanoscale diffraction and imaging techniques for high pressure sciences
• Novel Pressure-Induced Magnetic Transition in Magnetite (Fe3O4)
• Phase relations and density of iron at the Earth’s core conditions
• Stable Isotope Biogeochemistry of the Centennial Re-survey of the San Jacinto Mountains, CA
• Structure transition of Fe3-xTixO4 solid solution under pressures
• Synthesis of Coesite Nanocrystals from Periodic Mesoporous Organosilicas (PMOs) at High Pressure and Temperature
• The Adsorption of Short Single-Stranded DNA Oligomers on Mineral Surfaces
• Ultrastability and Size-dependent High Pressure Behavior in Nanoscale Y2O3
• Weathering in the late Archean and perturbations by oxygenic photosynthesis (Invited)
• A High-Pressure Study of the NH3-H2 System
• Beyond Band Theory for Minerals at High Pressures (Invited)
• Carbon Cycle in the Subduction Zone and Deep Mantle: Constraints from Equilibrium Experiments at High Pressure and Temperature (Invited)
• Carbonate melts in the Earth's mantle
• Climate of Australia over the past 100 ka inferred from stable isotopes in avian eggshells (Invited)
• Comparative compressibility of hydrous wadsleyite
• Complexity of Arsenate Adsorption at Iron and Aluminum Oxide-Water Interfaces
• Constraints on the Composition of the Earth's Liquid Outer Core from Shock Wave Density and Sound Velocity Measurements
• Crystal chemistry of Fe(III)-bearing magnesium silicate perovskite
• Cubic silicon carbide and boron nitride as possible primary pressure calibrants for high pressure and temperature scale
• Effects of Fe-Enrichment on the Equation of State and Stability of (Mg,Fe)SiO3 Perovskite and Post-Perovskite
• Elastic isotropy of iron under core conditions and other recent advances (Invited)
• Elasticity of cubic boron nitride under ambient condition
• Energy-Dispersive X-ray Diffraction Investigation of Amorphous Lithium Borate Structure: A Demonstration of the Paris-Edinburgh Cell Setup at 16BM-B at the APS
• Equilibrium between solid and liquid iron: The Fe-Si-O system at high pressures
• Experimental evidence for iron enrichment in (Mg,Fe)SiO3 post-perovskite relative to perovskite
• Factors affecting the hydrogen isotopic composition of dissolved organic matter along a salinity gradient
• Hemispherical Anisotropic Patterns of the Earth's Inner Core
• High pressure synchrotron x-ray powder diffraction and infrared spectroscopy study on brucite
• High-pressure Raman spectroscopic study of magnetite Fe3O4
• High-pressure polymorphs of iron-rich (Mg, Fe)SiO3 and FeGeO3 perovskite and post-perovskite. Takamitsu Yamanaka1, Wendy L. Mao2, P. Ganesh1, Luke Shulenburger1, Ho-kwang Mao1 and Russell J. Hemley1 1Geophysical Laboratory, Carnegie Institute of Washington, Washington, D.C. 20015 2 Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305
• Influence of speciation of C-O-H-N volatiles in silicate melts and coexisting fluids on C and N solubility in melts and on C and N isotope fractionation between melt and coexisting fluid to upper mantle pressure and temperature as a function of redox conditions
• Isotope fractionation during core formation (Invited)
• Life detection at a Mars analogue site of present-day serpentinization in the Tablelands Ophiolite of Newfoundland (Invited)
• Molybdenite Mineral Evolution: A Study Of Trace Elements Through Time
• New Capabilities and Challenges for Mineral Microanalysis using Large Area Silicon-Drift Detectors on Field Emission SEM's and Electron Microprobes
• Nitrate isotope fractionations during biological nitrate reduction: Insights from first principles theoretical modeling
• Oxygen and silicon partitioning between molten iron and silicate melts
• Phase equilibria in the FeO-Fe2O3-NiO-H2S-H2O-HCl system: An experimental study with implications for the stability of Ni-bearing phases at ultramafic-hosted hydrothermal systems
• Quantitative Investigation of Post-Burial H Isotope Exchanges in Organic Molecules
• Solution behavior of C-O-H volatiles in silicate melts under upper mantle pressures and temperatures as a function of redox conditions
• Solution of helium in SiO2 glass and its effect on the glass structure at high pressure
• Strength of diamond at high pressure from shock wave experiments
• The effect of temperature and pressure on optical absorption spectra of transition zone minerals - Implications for the radiative conductivity of the Earth's interior
• Thermal Conductivity Measurements of Periclase (MgO) at High Pressure and Temperature using Time Domain Thermoreflectance
• Thermal Conductivity of Argon at High Pressures and High Temperatures
• Tracking the Evolution of FE-,TI-OXIDE Phase Changes in Microbial Fossilization Experiments: Understanding the Role of Microbes in Diagenesis
• Using Carbon and Nitrogen Isotopic Ratios as Paleoclimate Proxies in Baffin Island Lakes
• Visualizing Earth's Core-Mantle Interactions using Nanoscale X-ray Tomography
• Water-CO2 Mixtures Under Extreme Conditions
• <SUP>2</SUP>H and <SUP>1</SUP>H NMR study on hydrogen isotope effects in silicate glasses
• Algal pigments record shifts in dominant primary productivity through the Holocene in an arctic lake
• Biosynthesis and Isotopic Composition of Bacteriochlorophyll a and Okenone in Purple Sulfur Bacteria
• Brillouin Scattering and X-ray Diffraction of Argon to 65 GPa and 800 K
• COMPRES X-ray beamlines (X17B3 and X17C) for the diamond anvil cell at the National Synchrotron Light Source
• Carbon Speciation and Precipitation in C-O-H System at High Temperature and Pressure
• Carbon-bearing silicate melts in the deep Earth
• Complementary Vibrational Spectroscopy Investigations of Iron and Iron-Bearing Minerals (Invited)
• D/H isotopic fractionation effects in the H<SUB>2</SUB>-H<SUB>2</SUB>O system: An in-situ experimental study at supercritical water conditions
• Density and structure of jadeite melt at high pressure and high temperature
• Development on novel high pressure synchrotron radiation techniques at HPSynC
• Dynamic melting of metals in the diamond cell: Clues for melt viscosity?
• Electrical and Thermal Conductivity of Iron and Iron-Silicon Alloy at High Pressures
• Electrical resistivity of iron at high pressure and high temperature
• Electronic Spin Transition of Iron in Dense Hydrous Magnesium Silicate Phase D at High Pressure
• Experimental Evidence for a High Temperature Iron Isotope Fractionation
• Experimental evidence for Nd-Sr decoupling during low-temperature (20-170<SUP>o</SUP>C) hydrothermal alteration of olivine and clinopyroxene
• Experimental pressure enhancement of the rate of homogenous methanogenesis: implications for abiotic methane yields in terrestrial and planetary environments
• First-principles calculation of lattice thermal conductivity of (MgxFe1-xO)ferropericlase at lower mantle conditions
• High P-T Thermal Conductivity of Periclase using an Ultrafast Pump-Probe Method
• High pressure constraints core formation from x-ray nanoscale tomography
• Hydrogen isotope analysis of amino acids and whole cells reflects biosynthetic processing of nutrient- and water-derived hydrogen
• Internally consistent pressure scale for Au, Pt, Mo, MgO, NaCl and Ne to 2.5 Mbar
• Low voltage and low overvoltage x-ray nanoanalysis with field emission electron microprobes and SEMs: Problems in quantitation for first-row transition elements
• Mercury (Hg) mineral evolution: Supercontinent assembly, ocean geochemistry and the terrestrial biosphere
• Microbial Ecology at an Arctic Geothermal Spring
• Microbial Nitrogen and Sulfur Cycles at the Playa and Playa-lake Deposits of White Sands National Monument, New Mexico
• Partitioning of Nb Between Rutile and Aqueous Fluid at High Pressures and Temperatures
• Petrological and experimental study of the effect of Fe on the stability of dolomite and magenesite in subduction zone
• Phase relations in chromite+SiO<SUB>2</SUB> system at high pressure and high temperature and implication for the origin of coesite bearing chromite
• Photosynthesis within Mars' volcanic craters?: Insights from Cerro Negro Volcano, Nicaragua
• Pressure-induced phase transitions and electron spin state changes in iron-bearing spinels
• Quantum Monte Carlo Computations of Phase Stability, Equations of State, and Elasticity of High-Pressure Silica
• Raman Spectroscopic Studies of Water-Carbon Dioxide Mixtures at High Pressure
• Science Planning for the New Research Vessel R/V Sikuliaq
• Single-Crystal X-Ray Diffraction of Forsterite to 90 GPa
• Sound velocity measurements of hcp-Fe at high pressure and high temperature: assessing the limits of the Birch's law
• Temperature Dependent Mössbauer Spectra of Aluminous Perovskite and Implications for the Earth's Lower Mantle
• The co-evolution of Fe-,Ti-oxides and other microbially induced mineral precipitates in sandy sediments: understanding the role of microbes in diagenesis
• The effects of iron and water on elastic properties of ringwoodite from theory and experiment: Constraint on chemical and thermal variations in the transition zone
• The formation of organic molecules in solar system environments: The Miller-Urey Experiment in Space preflight overview
• The phase relations in Earth's mid-lower mantle: constraints from in-situ XRD and quantitative chemical analysis
• Thermal equation of state of Fe(III) and Al-bearing magnesium silicate perovskite
• Time-Domain X-ray Diffraction in the Pulsed Laser Heated Diamond Anvil Cell
• Tracing bacterial metabolism using multi-nuclear (1H, 2H, and 13C) Solid State NMR: Realizing an Idea Initiated by James Scott
• Tracing the Origins of Organic Matter in the Ice of Svalbard, Norway
• View planetary differentiation process through high-resolution 3D imaging
• Visible and near-infrared reflectivity of solid and liquid methane: application to spectroscopy of Titan's hydrocarbon lakes
• An integral approach to investigate planetary cores
• Bridging the gap between static and dynamic compression: an inertial confinement approach to laser heating experiments in the diamond-anvil cell
• Bulk Earth carbon and its isotopic value
• Carbon diffusion in solid iron as function of pressure and temperature
• Combustion of organic matter in Mars analogs using SAM-like techniques
• Could borate have played a role in the RNA World?
• Density comparison between liquid and solid phases in the Fe-FeS system by the sink/float method: Implications for the structural evolution of the cores
• Development for sound velocity and density measurements of liquid metal at high pressures
• Elasticity and structure of sodium disilicate glass at high pressures and high temperatures
• Electron spin transition causing structure transformations of earth's interiors under high pressure
• Experimental determination of carbon partitioning between upper mantle minerals and silicate melts: initial results and comparison to trace element partitioning (Nb, Rb, Ba, U, Th, K)
• Formation of iron melt channels in silicate perovskite at Earth's lower mantle conditions
• High Resolution Quantitative Microbeam Analysis of Ir-coated Geological Specimens Using Conventionally Coated Standards
• Hydrogen isotope fractionation between C-H-O species in magmatic fluids
• In situ Raman study of dissolved CaCO<SUB>3</SUB> minerals under subduction zone conditions
• In-situ single-crystal structural determination of individual grains of high pressure phases in (Mg,Fe)SiO3 at deep lower mantle conditions
• In-situ, high pressure and temperature experimental determination of hydrogen isotope fractionation between coexisting hydrous melt and silicate-saturated aqueous fluid
• Microbes: Agents of Isotopic Change
• Microbial Cycling of Nitrogen and Carbon in AN Arctic Travertine Spring (jotun Spring, Svalbard Archipelago)
• Mineral evolution of redox-sensitive elements
• Origin of Metallization of FeO at High Temperatures and Pressures from First-principles DFT-DMFT Computations
• Pallasites as a proxy for understanding core-mantle partitioning
• Phase diagram of methane at high pressures and temperatures
• Phase relations and sound velocity measurements of iron-sulfur systems at high pressure: implications for the Earth's inner core
• Radiative Heat Transfer in a Hydrous Transition Zone
• SAM-like Evolved Gas Analysis of Mars Analog Samples from the Arctic Mars Analog Svalbard Expedition: Implications for Analyses by the Mars Science Laboratory
• Solubility and solution mechanisms of chlorine in aluminosilicate melts at high pressure and high temperature
• Sound velocity measurements on iron at high pressure and high temperature: an experimental test of the Birch's law
• Stable isotope fractionation at a glacial hydrothermal field: implications for biogeochemistry and biosignatures on Mars
• Strain and composition distribution study under high pressure at nanoscale
• Structure and Crystal Chemistry of FeAlO<SUB>3</SUB> at High Pressure
• Structure evolution of HoMnO3 under pressure
• Structure stability of iron phosphides and metal/silicate partition coefficient for phosphorus in early Mars
• Structure-property relationships of (C-O-H)-saturated silicate melt coexisting with silicate-saturated C-O-H fluid at high temperature and pressure and with variable redox conditions
• Synchrotron Mössbauer study of Fe-bearing pyrope at high pressures and temperatures
• Synthesis of a new high-pressure and high-temperature iron oxide, Fe<SUB>4</SUB>O<SUB>5</SUB>, a plausible key player in deep subduction processes
• The Effect of Si on the Melting Temperature of Iron up to 24 GPa
• The Effects of Spin Transition on Iron Diffusion in Ferropericlase
• The solubility of Nb-bearing rutile in aqueous fluids containing Albite, NaCl and NaF from 1-5 GPa and 300-600oC
• Warming Alters the Routing of Labile and Slower-Turnover Carbon Through Distinct Microbial Groups in Boreal Forest Organic Soils
• A new high-pressure phase of Fe2SiO4 and the relationship between spin and structural transitions
• Back-Transformation kinetics in the MgSiO3 system at upper mantle conditions
• Biogeochemistry of the sulfur oxidizer Thiomicrospira thermophila
• Complementary Vibrational Spectroscopy Investigations of Iron and Iron-Bearing Minerals (Invited)
• Constraints on the Properties of the Moon's Outer Core from High-Pressure Sound Velocity Measurements on Fe-S Liquids
• Data-Driven Abductive Discovery in the Earth Sciences (Invited)
• Disproportionation of (Mg,Fe)SiO3 into MgSiO3 perovskite and an Fe-rich hexagonal silicate in the deep lower mantle
• Ecologically and Geologically Relevant Isotope Signatures of C, N, and S in Okenone Producing Purple Sulfur Bacteria
• Effects of Pressure on the Short-range Structure and Speciation of Fluid phases in Silicate Melts: Insights from Multi-nuclear NMR and X-ray Raman Scattering
• High pressure and temperature electrical resistivity of iron and implications for planetary cores (Invited)
• High-Temperature Equilibrium Isotope Fractionation of Non-Traditional Stable Isotopes: Experiments, Theory, and Applications (Invited)
• Hydrogen in Earths Lowermost Mantle
• In situ X-ray observations of the melting relations in the Fe-S-H system under high pressure and high temperature
• Interaction of ribonucleotides with oxide and silicate minerals under varying environmental conditions
• Isotopic signatures associated with growth and metabolic activities of chemosynthetic nitrate-reducing microbes from deep-sea hydrothermal vents
• Light element controlled iron isotope fractionation in planetary cores
• Low viscosity of carbonate melts determined by falling sphere viscometry using ultrafast x-ray imaging at high pressures up to 6 GPa
• Mass Independent Fractionation of Hg Isotopes Preserved in the Precambrian
• Melting and chemical reactivity of hydrocarbons under high pressure and temperature
• Methane and ethane at high pressures: structure and stability
• Mineralogical Evidence for Subsurface Oxygenation Following the Great Oxidation Event
• Nanoscale Origin of the Dichotimous Viscosity-Pressure Behavior in Silicate Melts
• New Developments for Synchrotron High-PT XRD Studies using Laser-heated DAC at 16IDB HPCAT
• Non-Cubic Power-law Scaling of Density in Metallic Glasses (Invited)
• Pressure effect on the elasticity and structure of Na- silicate glasses
• Probing the Hydrogen Sublattice of FeHx with High-Pressure Neutron Diffraction
• Rapid carbon-carbon bond formation and cleavage revealed by carbon isotope exchange between the carboxyl carbon and inorganic carbon in hydrothermal fluids
• Sound velocity of ? iron at Moon's core conditions
• Strategies for Analyzing Sub-Micrometer Features with the FE-EPMA
• Stress- and pressure-induced iron spin-state crossover in lower mantle minerals
• The effect of temperature and surface area on Sr, Ba and REE fractionation during low temperature serpentinization
• Thermal Equation of State of Iron: Constraint on the Density Deficit of Earth's Core
• Tourmaline in the 3.7-3.8 Ga Isua Supracrustal Belt, West Greenland - A window to Boron Concentrations in the Eoarchean Eon
• Toward comprehensive studies of liquids at high pressures and high temperatures: Integration of structure and property measurements in a Paris-Edinburgh cell (Invited)
• Toward measurements of volatile behavior at realistic pressure and temperature conditions in planetary deep interiors. (Invited)
• Trace element partitioning in Fe-P-O-S alloy systems
• Vibrational, elastic, and structural properties of cubic silicon carbide under pressure up to 75 GPa and temperature up to 773K: implication for a primary pressure scale
• "Invar"-like behavior in compressed Fe<SUB>7</SUB>C<SUB>3</SUB> with implication for deep carbon cycle
• Application of multigrain crystallography to mineralogy of the deep Earth
• Can Suspended Iron-Alloy Droplets Explain the Origin, Composition and Properties of Large Low Shear Velocity Provinces?
• Consequences and Resolution of Lunar Lower Mantle Partial Melt
• Crystal Structure of Calcium Silicate Perovskite Synthesized under Water Saturated Conditions at Mantle Related Pressure-Temperature
• Disproportionation of (Mg,Fe)SiO<SUB>3 </SUB>Perovskite and its Implications to the Deep Earth
• Effects of chemical composition on the environments of D<SUP>+</SUP> and H<SUP>+</SUP> in alkali silicate glasses: with implications for D/H fractionation in magmatic processes
• Elasticity and Anelasticity of Materials from Time-Resolved X-ray Diffraction
• Growth Kinetics of a Reaction Rim Between Iron and Graphite/Diamond and the Carbon Diffusion Mechanism at High Pressure and Temperature
• How is Mercury's dynamo powered?
• In-situ measurements of D/H fractionation between melt and coexisting aqueous fluids in the Na<SUB>2</SUB>O-Al<SUB>2</SUB>O<SUB>3</SUB>-SiO<SUB>2</SUB>-H<SUB>2</SUB>O system
• Sulfur isotopic fractionation during planetary differentiation
• Water in Al-free Stishovite up to 65 GPa and 2000 K
• Alternative hypothese for the origin of the ultra-low velocity zones
• Apparatus and Techniques for Time-resolved Synchrotron X-ray Diffraction using Diamond Anvil Cells
• Applications of sample nanofabrication in diamond-anvil cell experiments
• Behavior of basalt-carbonate melts at high pressures
• Crystal Structure of Pure and Aluminous Calcium Silicate Perovskites at Mantle Related Pressure and Temperature
• Equations of state and phase transitions in (Mg,Fe)SiO3 perovskite and post-perovskites, position of the phase boundary and its double crossing, by Quantum Monte Carlo
• High-pressure thermal properties of liquid, solid and amorphous H<SUB>2</SUB>O
• Low Fe<SUP>3+</SUP> in Bridgmanite and Possible Existence of an Oxidizing Layer in the Mid Mantle
• Magnetic phase diagrams and thermal equations of state of Fe<SUB>7</SUB>C<SUB>3</SUB> and Fe<SUB>3</SUB>C up to the pressure-temperature conditions of Earth's core
• Probing iron spin state by optical absorption in laser-heated diamond anvil cell
• Stable Isotope Evidence for Planetary Differentiation
• Synthesis of Xenon and Iron/Nickel Intermetallic Compounds Under the Thermodynamic Conditions of the Earth's Core.
• Viscosity and mixing between K and alkaline-earth silicate melts
• Viscosity of liquids sulfur and selenium at high pressures and high temperatures and their correlations with liquid structure
• Advanced Synchrotron Technique for Synthesis and Analysis of Polyhydrides in the Laser Heated Diamond Anvil Cell
• Direct thermal conductivity measurements on metals at high pressure and temperature: from the usual to the unusual
• Discrete stages of core formation survive the Moon-forming impact
• Early geodynamo powered by magnesium exsolution?
• Effects of Pressure and Temperature on the Kinetics of Iron-magnesite Redox Reaction: Implication for the Genesis of Ultradeep Diamonds
• Experimental investigation of Fe<SUP>3+</SUP>- rich majoritic garnet and improvement of the majorite geobarometer
• Experimental observations of a<SUB>TiO2</SUB> in rutile-undersaturated silicate melts and implications for estimating a<SUB>TiO2</SUB> in natural systems
• Is the Silicate Perovskite to Post-Perovskite Transition Boundary Consistent with Earth's D'' Discontinuity?
• Mechanism and thermodynamics of the high- to low-spin transition in (Mg,Fe)O ferropericlase: An experimental null result
• Metastability of Subducted Slabs in the Mantle Transition Zone: A Collaborative Geodynamic, Petrologic, and Seismological Approach
• Mg-carbonate interaction with metallic iron in the lower mantle and at the core-mantle boundary
• New FeO<SUB>2</SUB> phase and the origins of ultralow-velocity zones at the core-mantle boundary
• Noble Gas Recycling: Experimental Constraints on Ar, Kr, and Xe Solubility in Serpentinite
• Noble Gases Trace Earth's Subducted Water Flux
• On the Origin of High Shear Wave Velocities in the Deep Roots of Cratons
• Plate Tectonic Cycling and Whole Mantle Convection Modulate Earth's <SUP>3</SUP>He/<SUP>22</SUP>Ne Ratio
• Radiative conductivity and abundance of post-perovskite in D''
• Synthesis of FeO<SUB>2</SUB> and the Fe-O-H system in the deep Earth
• The Effect of Carbon on the Dihedral Angle of Metallic Melt with Implications for the Timing and Efficiency of Core Formation
• The Influence of Wavelength-Dependent Absorption and Temperature Gradients on Temperature Determination in Laser-Heated Diamond-Anvil Cells
• Ultrahigh-pressure structure of GeO<SUB>2</SUB> glass with coordination number &gt;6: implications for structure of magma at the core-mantle boundary
• Cristobalite X-I: A bridge between low and high density silica polymorphs
• Curiosity and the Four Seasons: In Situ Measurements of the Atmospheric Composition over Three Mars Years
• Data-driven exploration of copper mineralogy and its application to Earth's near-surface oxidation
• Detecting Kerogen as a Biosignature Using Co-located UV Time-Gated Raman and Fuorescence Spectroscopy
• Electron Density Distribution Changes of Magnesiowüstite With Pressure
• Experimental Evidence of Low Density Liquid Water under Decompression
• Experimental evidence of body centered cubic iron in Earth's core
• Experimental study and thermodynamic modeling of the phase relation in the Fe-S-Si system with implications for the distribution of S and Si in a partially solidified core
• Five Years of Analyses of Volatiles, Isotopes and Organics in Gale Crater Materials
• Geochemical Characterization Of Cherts From The 3.46Ga Apex Basalt To Assess The Origins Of Possible Biosignatures
• Hydrothermal Signatures at Gale Crater, Mars, and Possible In-Situ Formation of Tridymite
• Is Mars Dead and Does it Matter: The Crucial Scientific Importance of a Lifeless Mars
• Linking paleointensities and exsolution-driven dynamo
• Mars Methane at Gale Crater Shows Strong Seasonal Cycle: Updated Results from TLS-SAM on Curiosity
• Na, Rb and Cs partitioning between metal, silicate and sulfide: Implications for volatile depletion in terrestrial planets
• Network Analysis of Earth's Co-Evolving Geosphere and Biosphere
• Nitrogen and Martian Habitability: Insights from Five Years of Curiosity Measurements
• No Radiative Heat Transport Through Pyrolitic Lower Mantle
• Origin of the Lower-Mantle Heterogeneities - Importance of the Crystal Chemistry of Bridgmanite
• Pulsed Laser Techniques to Determine Lattice and Radiative Thermal Conductivity of Deep Planetary Materials at Extreme Pressure-Temperature Conditions
• Rapid reduction of MORB glass in piston cylinder experiments with graphite capsule - a XANES study
• Recent select Sample Analysis at Mars (SAM) Testbed analog results
• Rutilated quartz: combining Ti-in-quartz thermometry and lattice diffusion
• SHERLOC on Mars 2020
• Sequestration of nitrogen in the core during accretion
• The Rise of Oxygen in the Earth's Atmosphere Controlled by the Efficient Subduction of Organic Carbon
• The Solidus of Mar
• Timing the oxidation of Earth's crust: Evidence from big data records of manganese mineralization
• Visualizing Complex Environments in the Geo- and BioSciences
• A new high speed and large capacity centrifuge for experimental petrology study at high pressure and temperature
• Characterizing X-ray Amorphous Phases through Diffraction Profile Modeling: Understanding Weathering and Diagenesis in Gale Crater
• Constraining elemental trends in Raman spectra of terrestrial and extraterrestrial insoluble organic matter samples
• Data-Driven Discovery and the Rise of the Collaborative Culture of Data Sharing
• Direct measurements of thermal conductivity of deep Earth materials via pulsed laser techniques in a laser heated diamond anvil cell
• Early episodes of high-pressure core formation preserved in plume mantle
• Evaporation induced Cu isotope fractionation during tektite formation
• Evidence for Alteration and Diagenesis at Gale Crater, Mars from the Curiosity Rover
• Global Earth Mineral Inventory : A DCO Data Legacy
• Interstitial Carbon in Solid Fe at High Pressures: Implication to Carbon Content in the Earth's Inner Core
• Mobility of CaCO<SUB>3</SUB> in Subduction Zones
• Multi-Technique Analysis of "Synthetic" Extraterrestrial Analogs as Test-bed for Detection of Molecular Biomarkers in Planetary Contexts
• New Bond-Valence Parameters for Inferring the Oxidation State of Transition Metals in Sulfide and Sulfosalt Minerals.
• Nitrogen systematics in thermally altered insoluble organic matter: An experimental study
• Predicting Multi-Component Mineral Compositions in Gale crater, Mars with Label Distribution Learning
• Refractive Index Measurements of a Solar System Organic Analog
• Reworking and Diagenesis of Martian Soil: Pathway to Murray Formation Sediments?
• SAM and the organic matter in Gale Crater, Mars - Inventory and implications
• Silicon Abundance in the Earth's Core Constrained by a Multi-Technique Approach
• Strain-rate and temperature effects on kinetics of phase transitions in albite
• Structural measurement on 60 mol% Al<SUB>2</SUB>O<SUB>3</SUB> - 40 mol% SiO<SUB>2</SUB> glass up to 131 GPa
• Temperature-induced amorphization in CaCO<SUB>3 at high pressure</SUB>: Implication for recycled CaCO<SUB>3</SUB> in the transition zone
• The Deep Carbon Observatory: The Carnegie Institution for Science as a Global Center for Collaborative and Interdisciplinary Research
• The Mineralogical Record of Redox at Gale Crater
• Thermal Conductivity at the Base of the Earth's Lower Mantle
• Thermal conductivity of iron in Earth's core is low enough to support thermal convection
• Transport Properties of Fe at Earth's Core Conditions: Agreement between Experiment and Theory
• Unfinished Business: Constraints on Evolution of the Lunar Crust
• Calcite Phase Transitions and Melting Under Shock Loading and Release Using Ultrafast X-Ray Diffraction
• Carbon Isotope Fractionation between CO<SUB>2</SUB> and Carbonate Melt, an Experimental Approach
• Copper and Oxygen Isotope Fractionation Due to Partial Vaporization of Rhyolitic and Basaltic Melts
• Creating, Managing and Evaluating Data Legacies : Updates on the Global Earth Mineral Inventory.
• Data-driven discovery in mineralogy: Insights from natural kind clustering
• Deep Focus Earthquakes, Deep Slab Fluids, and Superdeep Diamonds
• Density of Hydrous Silicate Melts in the Transition Zone
• Excess oxygen in ferric oxide and unexpected chemistry of mantle oxygen
• Exploring carbon mineralogy and mineral evolution through deep time with advanced analytics and visualization
• Formation of akaganeite in Gale crater, Mars
• Glen Torridon: Chemical Relationship to Members of the Murray Formation (Gale Crater, Mars)
• Hydrogen isotope fractionation within silicate melts - First experimental results on the pressure and temperature dependency of D/H molar volume isotope effects
• In-Situ Alteration of Organic Biosignatures in Perchlorate-Spiked Martian Regolith Analog
• Interactive, Web-based Visualizations for Hierarchical Information and Knowledge in Geosciences: An Implementation on the Dana Classification and its Applications
• Melting above the mantle transition zone beneath the Pacific margins
• Mineral evolution, natural kinds, and the origins of life
• Mineralogical evidence for water-rock interactions in ancient Gale crater, Mars from the CheMin instrument on the Curiosity rover
• Natural clustering of pyrite with implications for its formational environment
• Natural kind clustering of presolar silicon carbides and its astrophysical implications
• Novel experimental approach to thermal conductivity measurements of materials using continuous and pulsed laser system with Pockels cell
• Open science at AGU Publications: an update on open access, preprints, and FAIR data developments
• Predicting unknown mineral localities based on mineral associations
• Pressure effect on the oxidation state of a terrestrial magma ocean, from experimental perspective
• Pulsed electrical melting of transition metals in diamond anvil cells: a new probe to determine the Earth's core temperature
• Stress induced interconnection of core-forming melt in a bridgmanite matrix
• Synthesizing carbon mineralogy: Insights on forms, quantities, and origins
• The Clay Minerals of Glen Torridon
• The Deep Carbon Observatory: An Interdisciplinary Quest to Study Carbon in Earth
• The effects of hydration and silica enrichment on the seismic velocity structure of the continental mantle lithosphere
• The redox boundaries and volatiles cycle of Earth's interior through space and time
• Tracking the evolution of our planet using large scale geochemistry and metagenomic data
• Transfer of SiO<SUB>2</SUB> from the core to the mantle and its fate in the Earth in early and present times
• Wet and Deep vs. Dry and Shallow: Global Fractionation Conditions in Volcanic Arcs
• A machine learning geobarometer for diamond-hosted majoritic garnet inclusions
• Electrical resistivity measurement of pure iron in the multi-anvil press: discussions on different techniques.
• New method to investigate interconnection of core-forming metallic melt in a solid silicate matrix
• Quantifying the water content in dense SiO<SUB>2</SUB>
• Sample Chemistry Revealed by TMAH-Evolved Gas Analysis: Results from the First In Situ Thermochemolysis Experiment at Gale Crater, Mars
• The IRH-DAC: Resistive Heating of Non-Metallic Samples to 3000 K at 50 GPa in the Diamond Anvil Cell
• The stability of subducted glaucophane with the Earths secular cooling
• X-ray imaging to study compaction under high pressures
• A Novel Framework for Assessing Semantic Information in Planetary Atmospheres for Habitability and Biosignatures
• Can we use network science to identify planetary biosignatures?
• New Estimates of Nitrogen Fixation on Early Earth
• Predicting Nitrogen Isotope Evolution on Mars

Linked Collaborating Authors [?]

• A. Steele
• Anirudh Prabhu
• Danica Adams
• Haemyeong Jung
• J. R. Brucato
• Kanani K. M. Lee
• P. M. Bremner
• Rainer Schräpler
• S. M. Morrison
• Taehyun Kim
• Teresa Fornaro
• Vincenzo Stagno
• Vitali B. Prakapenka
• Yoonah Bang