What is he best known for?
The fields of study he is best known for:
- Oxygen
- Mineral
- Organic chemistry
His primary areas of investigation include Mineralogy, Analytical chemistry, Geochemistry, Partial melting and Fugacity.
His research integrates issues of Phase, Mineral redox buffer, Bar, Silicate and Magma in his study of Mineralogy.
His research in Analytical chemistry intersects with topics in Magma chamber, Carbon dioxide and Aqueous solution.
His work carried out in the field of Carbon dioxide brings together such families of science as Carbonate and Solubility.
In general Geochemistry study, his work on Syenogranite and A-type granite often relates to the realm of Hypersolvus, thereby connecting several areas of interest.
His Partial melting research integrates issues from Amphibole and Peridotite.
His most cited work include:
- Experimental determination of the fluid-absent melting relations in the pelitic system (889 citations)
- Origin of an A-type granite; experimental constraints (623 citations)
- An Experimental Study of Water and Carbon Dioxide Solubilities in Mid-Ocean Ridge Basaltic Liquids. Part I: Calibration and Solubility Models (597 citations)
What are the main themes of his work throughout his whole career to date?
John R. Holloway focuses on Mineralogy, Analytical chemistry, Geochemistry, Solubility and Mantle.
His studies deal with areas such as Partial melting, Phase, Liquidus, Mineral redox buffer and Silicate as well as Mineralogy.
The study incorporates disciplines such as Anhydrous, Oxygen and Aqueous solution in addition to Analytical chemistry.
His work in Geochemistry addresses subjects such as Muscovite, which are connected to disciplines such as Kyanite.
As part of one scientific family, John R. Holloway deals mainly with the area of Solubility, narrowing it down to issues related to the Carbon dioxide, and often Silver oxalate.
His Mantle study deals with Olivine intersecting with Spinel.
He most often published in these fields:
- Mineralogy (45.38%)
- Analytical chemistry (33.85%)
- Geochemistry (25.38%)
What were the highlights of his more recent work (between 2003-2013)?
- Geochemistry (25.38%)
- Mineralogy (45.38%)
- Environmental science (3.85%)
In recent papers he was focusing on the following fields of study:
John R. Holloway mainly focuses on Geochemistry, Mineralogy, Environmental science, Mantle and Hydrothermal circulation.
John R. Holloway combines subjects such as Zoisite, Amphibole and Oceanic crust with his study of Geochemistry.
He has included themes like Solubility, Wüstite, Peridotite and Liquidus in his Mineralogy study.
His study in Mantle is interdisciplinary in nature, drawing from both Brittleness, Martian, Olivine and Analytical chemistry.
His Analytical chemistry research includes elements of Wide dynamic range, Mineral redox buffer and Abbe refractometer.
His Hydrothermal circulation research incorporates themes from Saponite, Clay minerals, Illite and Montmorillonite.
Between 2003 and 2013, his most popular works were:
- Colonization of nascent, deep-sea hydrothermal vents by a novel Archaeal and Nanoarchaeal assemblage. (56 citations)
- Manufacture of robust surface plasmon resonance fiber optic based dip-probes (54 citations)
- Simulating the Earth: Experimental Geochemistry (49 citations)
In his most recent research, the most cited papers focused on:
The scientist’s investigation covers issues in Mineralogy, Surface plasmon resonance, Optical fiber, Refractive index and Spectroscopy.
His work deals with themes such as Catalysis and Organic synthesis, which intersect with Mineralogy.
His Localized surface plasmon study, which is part of a larger body of work in Surface plasmon resonance, is frequently linked to Sputter deposition, Reproducibility and Derivative, bridging the gap between disciplines.
His Optical fiber research incorporates elements of Wide dynamic range, Abbe refractometer and Analytical chemistry.
Among his Spectroscopy studies, you can observe a synthesis of other disciplines of science such as Solubility, Crystal growth, Solid solution, Atmospheric pressure and Mineral redox buffer.
This overview was generated by a machine learning system which analysed the scientist’s
body of work. If you have any feedback, you can
contact us
here.
