A5040243049- Geological and Geochemical Analysis
- High-pressure geophysics and materials
- earthquake and tectonic studies
- Astro and Planetary Science
- Geochemistry and Geologic Mapping
- Planetary Science and Exploration
- Glass properties and applications
- Hydrocarbon exploration and reservoir analysis
- Mineralogy and Gemology Studies
- Catalytic Processes in Materials Science
- Crystal Structures and Properties
- Thermal and Kinetic Analysis
- Building materials and conservation
- Pleistocene-Era Hominins and Archaeology
- Advanced Chemical Physics Studies
- Phase Equilibria and Thermodynamics
- Geology and Paleoclimatology Research
- Catalysis and Oxidation Reactions
- Geochemistry and Elemental Analysis
- Clay minerals and soil interactions
- Radioactive element chemistry and processing
- Spectroscopy and Laser Applications
- Metallurgical Processes and Thermodynamics
- Geomagnetism and Paleomagnetism Studies
- nanoparticles nucleation surface interactions
University of Oxford
2016-2025
University of Manchester
1972-2019
University of Bristol
1998-2018
Science Oxford
2012-2016
George Washington University
2014
National Museum of Natural History
2014
Smithsonian Institution
2014
Macquarie University
2006-2011
ARC Centre of Excellence for Core to Crust Fluid Systems
2011
Monash University
2004
The earth's mantle is degassed along mid-ocean ridges, while rehydration and possibly recarbonaton occurs at subduction zones. These processes the speciation of C-H-O fluids in are related to oxidation state peridotite. Peridotite xenoliths from continental localities exhibit an oxygen fugacity (fo(2)) range -1.5 +1.5 log units relative FMQ (fayalite-magnetite-quartz) buffer. lowest values zones extension. Highly oxidized (fo(2) greater than FMQ) come regions recent or acive (for example,...
As part of a project to investigate the volatilities so-called “moderately volatile elements” such as Zn, In, Tl, Ga, Ag, Sb, Pb, and Cl during planetary formation, we began by re-calculating condensation temperatures these elements from solar gas at 10-4 bar. Our calculations highlighted three areas where currently available estimates temperature could be improved. One is nature mixing behavior many important trace when dissolved in major condensates silicates, Fe-rich metals, sulfides....
The extent to which sulfur dissolves in silicate melts saturated an immiscible sulfide phase is a fundamental question igneous petrology and plays primary role the generation of magmatic ore deposits, volcanic degassing, planetary differentiation. In systems, can be described as FeS-NiS-CuS0.5 solutions with Fe/(Fe+Ni+Cu) significantly less than 1. Despite presence Ni Cu sulfide, however, most experimental studies date have concentrated on effects melt composition solubility used essentially...
Research Article| September 01, 1986 Structures, textures, and cooling histories of Columbia River basalt flows PHILIP E. LONG; LONG 1Geosciences Group, Basalt Waste Isolation Project, Rockwell Hanford Operations, Richland, Washington 99352 Search for other works by this author on: GSW Google Scholar BERNARD J. WOOD 2Department Geological Sciences, Northwestern University, Evanston, Illinois 60201 Author Article Information Publisher: Society America First Online: 01 Jun 2017 Online ISSN:...
We report new findings related to sample 14161,7373, the first analyzed limar intrusive rock show textural evidence for formation of granitic material by silicate liquid immiscibility (SLI) and geochemical separation that material, at least on a small scale, from mafic residua. Ion microprobe analyses rare-earth element (REE) concentrations in silicates record compositional evolution this late-stage assemblage. For whose bulk assemblage, whitlockite monzogabbro, has REE ~5-6× KREEP levels,...