What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Basalt
- Paleontology
Clark M. Johnson mainly investigates Geochemistry, Mineralogy, Isotope fractionation, Fractionation and Inorganic chemistry.
His is doing research in Diagenesis, Siderite, Pyrite, Banded iron formation and Weathering, both of which are found in Geochemistry.
His study focuses on the intersection of Mineralogy and fields such as Sedimentary rock with connections in the field of Total organic carbon, Archaeology and Prehistory.
His Equilibrium fractionation study, which is part of a larger body of work in Isotope fractionation, is frequently linked to Ferrous, bridging the gap between disciplines.
Clark M. Johnson has included themes like Seawater, Igneous rock and Analytical chemistry in his Fractionation study.
His Inorganic chemistry study combines topics from a wide range of disciplines, such as Ion exchange and Nuclear chemistry.
His most cited work include:
- Application of Fe isotopes to tracing the geochemical and biological cycling of Fe (443 citations)
- Kinetic and equilibrium Fe isotope fractionation between aqueous Fe(II) and Fe(III) (369 citations)
- The Iron Isotope Fingerprints of Redox and Biogeochemical Cycling in Modern and Ancient Earth (295 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Geochemistry, Isotope fractionation, Mineralogy, Fractionation and Analytical chemistry.
His research in Basalt, Mantle, Archean, Crust and Geochronology are components of Geochemistry.
His study looks at the relationship between Archean and fields such as Weathering, as well as how they intersect with chemical problems.
His studies examine the connections between Isotope fractionation and genetics, as well as such issues in Magnetite, with regards to Siderite.
His studies in Mineralogy integrate themes in fields like Sedimentary rock, Hydrothermal circulation and Banded iron formation.
His study in the fields of Ferric under the domain of Inorganic chemistry overlaps with other disciplines such as Goethite, Oxide and Ferrous.
He most often published in these fields:
- Geochemistry (61.81%)
- Isotope fractionation (36.22%)
- Mineralogy (31.10%)
What were the highlights of his more recent work (between 2014-2021)?
- Geochemistry (61.81%)
- Isotope fractionation (36.22%)
- Analytical chemistry (21.26%)
In recent papers he was focusing on the following fields of study:
His primary areas of investigation include Geochemistry, Isotope fractionation, Analytical chemistry, Fractionation and Archean.
His is involved in several facets of Geochemistry study, as is seen by his studies on Banded iron formation, Continental crust, Radiogenic nuclide, Mantle and Geochronology.
His Isotope fractionation research is multidisciplinary, incorporating elements of Environmental chemistry and Mineralogy.
His work carried out in the field of Analytical chemistry brings together such families of science as Isotopes of silicon and Particle size.
His Fractionation research includes themes of Inorganic chemistry and Hydrothermal circulation.
His research in Archean intersects with topics in Magnetite, Paleoarchean, Weathering, Precambrian and Oncolite.
Between 2014 and 2021, his most popular works were:
- Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (122 citations)
- Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (122 citations)
- Experimental calibration of Mg isotope fractionation between dolomite and aqueous solution and its geological implications (75 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Sedimentary rock
- Paleontology
His main research concerns Geochemistry, Isotope fractionation, Fractionation, Archean and Hydrothermal circulation.
His work on Radiogenic nuclide, Geochronology and Banded iron formation as part of his general Geochemistry study is frequently connected to Field, thereby bridging the divide between different branches of science.
The study incorporates disciplines such as Environmental chemistry and Hot spring in addition to Isotope fractionation.
When carried out as part of a general Fractionation research project, his work on Equilibrium fractionation is frequently linked to work in Iron oxide and Goethite, therefore connecting diverse disciplines of study.
His biological study spans a wide range of topics, including Precambrian and Weathering.
Clark M. Johnson has researched Hydrothermal circulation in several fields, including Mineralogy and Analytical chemistry.
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