Area of research
Geophysics · Mechanics of Materials
Research interest
Research interests include Geological and Geochemical Analysis, High-pressure geophysics and materials, earthquake and tectonic studies, and Hydrocarbon exploration and reservoir analysis.
Hydrothermal Properties of Geologic Fluids
Carbon in Earth's Interior
Absence of amorphous forms when ice is compressed at low temperature
Carbon sequestration during core formation implied by complex carbon polymerization
Fluids of the Lower Crust: Deep Is Different
The Behavior of Halogens During Subduction-Zone Processes
In situ carbon mineralization in ultramafic rocks: Natural processes and possible engineered methods
Implications for metal and volatile cycles from the pH of subduction zone fluids
Detection of liquid H<sub>2</sub>O in vapor bubbles in reheated melt inclusions: Implications for magmatic fluid composition and volatile budgets of magmas?
Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes up
The global range of subduction zone thermal structures from exhumed blueschists and eclogites: Rocks are hotter than models
The solubility of rocks in metamorphic fluids: A model for rock-dominated conditions to upper mantle pressure and temperature
Crystal chemical constraints on inter-mineral Fe isotope fractionation and implications for Fe isotope disequilibrium in San Carlos mantle xenoliths
Ultralow viscosity of carbonate melts at high pressures
Brines at high pressure and temperature: Thermodynamic, petrologic and geochemical effects
Dehydration melting and the relationship between granites and granulites
The Chemistry of Carbon in Aqueous Fluids at Crustal and Upper-Mantle Conditions: Experimental and Theoretical Constraints
Brine-assisted anatexis: Experimental melting in the system haplogranite–H2O–NaCl–KCl at deep-crustal conditions
Experimental determination of <scp><scp>CePO</scp><sub>4</sub></scp> and <scp><scp>YPO</scp><sub>4</sub></scp> solubilities in <scp><scp>H<sub>2</sub>O</scp></scp>–<scp><scp>NaF</scp></scp> at 800°<scp>C</scp> and 1 GPa: implications for rare earth element transport in high‐grade metamorphic fluids
Thermodynamic Modeling of Fluid-Rock Interaction at Mid-Crustal to Upper-Mantle Conditions
Global variations in H<sub>2</sub>O/Ce: 1. Slab surface temperatures beneath volcanic arcs
Zircon solubility and zirconium complexation in H2O+Na2O+SiO2±Al2O3 fluids at high pressure and temperature
A thermodynamic model for the system<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" altimg="si32.gif" overflow="scroll"><mml:mrow><mml:msub><mml:mrow><mml:mtext>SiO</mml:mtext></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:ms>–</mml:ms><mml:msub><mml:mrow><mml:mtext>H</mml:mtext></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mtext>O</mml:mtext></mml:mrow></mml:math>near the upper critical end point based on quartz solubility experiments at 500–1100
Abiogenic methanogenesis during experimental komatiite serpentinization: Implications for the evolution of the early Precambrian atmosphere