What is he best known for?
The fields of study he is best known for:
Hugh St. C. O'Neill mainly focuses on Mineralogy, Analytical chemistry, Silicate, Mantle and Olivine.
His Mineralogy research includes elements of Spinel, Basalt and Spinel lherzolite.
His Analytical chemistry research incorporates elements of Electrochemistry, Mineral redox buffer, Crystallization and Oxidation state.
As part of the same scientific family, Hugh St. C. O'Neill usually focuses on Silicate, concentrating on Stoichiometry and intersecting with Crystal and Oxide.
His Mantle research is multidisciplinary, incorporating perspectives in Chondrite and Formation and evolution of the Solar System.
His research in Olivine intersects with topics in Calcium content, Calcium, Composition dependence, Mole fraction and Magnesium.
His most cited work include:
- Cosmochemical Estimates of Mantle Composition (853 citations)
- Simple spinels; crystallographic parameters, cation radii, lattice energies, and cation distribution (519 citations)
- THE RELATIVE EFFECTS OF PRESSURE, TEMPERATURE AND OXYGEN FUGACITY ON THE SOLUBILITY OF SULFIDE IN MAFIC MAGMAS (481 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Analytical chemistry, Mineralogy, Olivine, Silicate and Mantle.
His Stoichiometry study, which is part of a larger body of work in Analytical chemistry, is frequently linked to Partition coefficient, bridging the gap between disciplines.
His work deals with themes such as Solid solution, Basalt, Fugacity and Spinel lherzolite, which intersect with Mineralogy.
Hugh St. C. O'Neill has included themes like Electron microprobe, Trace element, Spinel, Ionic radius and Forsterite in his Olivine study.
His study focuses on the intersection of Silicate and fields such as Sulfide with connections in the field of Saturation and Sulfur.
His work is dedicated to discovering how Mantle, Chondrite are connected with Formation and evolution of the Solar System and other disciplines.
He most often published in these fields:
- Analytical chemistry (42.08%)
- Mineralogy (38.25%)
- Olivine (28.42%)
What were the highlights of his more recent work (between 2015-2021)?
- Analytical chemistry (42.08%)
- Silicate (27.32%)
- Olivine (28.42%)
In recent papers he was focusing on the following fields of study:
Hugh St. C. O'Neill spends much of his time researching Analytical chemistry, Silicate, Olivine, Geochemistry and Forsterite.
His Analytical chemistry research is multidisciplinary, incorporating perspectives in Magnetite, Mineral redox buffer, Oxidation state and XANES.
Hugh St. C. O'Neill combines subjects such as Oxide, Doping, Mineral, Silicate glass and Anorthite with his study of Silicate.
His Olivine study deals with the bigger picture of Mineralogy.
His studies in Mineralogy integrate themes in fields like Sulfide, Thermodynamic model and Intermediate composition.
His Geochemistry study incorporates themes from Chondrite and Meteorite.
Between 2015 and 2021, his most popular works were:
- The effect of bonding environment on iron isotope fractionation between minerals at high temperature (58 citations)
- Petrogenesis and Geochemistry of Archean Komatiites (56 citations)
- A re-assessment of the oxidation state of iron in MORB glasses (49 citations)
In his most recent research, the most cited papers focused on:
His scientific interests lie mostly in Analytical chemistry, Mineral redox buffer, Olivine, Mantle and Partial melting.
The Analytical chemistry study combines topics in areas such as Magnetite, Mineralogy, Oxidation state and Liquidus.
His biological study deals with issues like Vanadium, which deal with fields such as Silicate.
Hugh St. C. O'Neill specializes in Mineralogy, namely Forsterite.
His Olivine study frequently links to adjacent areas such as Spinel.
His Mantle study introduces a deeper knowledge of Geochemistry.
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