What is he best known for?
The fields of study he is best known for:
- Mineral
- Carbon dioxide
- Sedimentary rock
Hiroshi Ohmoto mainly focuses on Geochemistry, Hydrothermal circulation, Inorganic chemistry, Pyrite and Felsic.
The various areas that Hiroshi Ohmoto examines in his Geochemistry study include Paleontology and Isotope geochemistry.
His work in the fields of Hydrothermal circulation, such as δ34S, overlaps with other areas such as Boiling-point elevation and Delta.
His study in the field of Equilibrium constant is also linked to topics like Dissociation constant.
He interconnects Seafloor massive sulfide deposits, Chalcopyrite, Sulfide, Continental crust and Solubility in the investigation of issues within Pyrite.
In his work, Mineralogy is strongly intertwined with Metamorphism, which is a subfield of Sedimentary rock.
His most cited work include:
- Isotopes of sulfur and carbon (1290 citations)
- SYSTEMATICS OF SULFUR AND CARBON ISOTOPES IN HYDROTHERMAL ORE DEPOSITS (895 citations)
- Stable isotope geochemistry of ore deposits (646 citations)
What are the main themes of his work throughout his whole career to date?
The scientist’s investigation covers issues in Geochemistry, Mineralogy, Hydrothermal circulation, Sulfur and Sulfide.
His work in Archean, Diagenesis, Pyrite, Sedimentary rock and Basalt are all subfields of Geochemistry research.
His Mineralogy study combines topics from a wide range of disciplines, such as Isotopes of carbon, Fluid inclusions, Weathering, Analytical chemistry and Seawater.
His work focuses on many connections between Hydrothermal circulation and other disciplines, such as Hematite, that overlap with his field of interest in Magnetite.
The concepts of his Sulfur study are interwoven with issues in Sulfate, Sulfate minerals, δ34S and Isotope fractionation.
His biological study spans a wide range of topics, including Inorganic chemistry, Equilibrium constant and Aqueous solution.
He most often published in these fields:
- Geochemistry (58.27%)
- Mineralogy (31.50%)
- Hydrothermal circulation (20.47%)
What were the highlights of his more recent work (between 2004-2021)?
- Geochemistry (58.27%)
- Archean (18.11%)
- Earth science (7.87%)
In recent papers he was focusing on the following fields of study:
Hiroshi Ohmoto spends much of his time researching Geochemistry, Archean, Earth science, Early Earth and Pilbara Craton.
His Basalt, Great Oxygenation Event, Weathering, Sedimentary rock and Banded iron formation investigations are all subjects of Geochemistry research.
His Weathering research also works with subjects such as
- Red beds which is related to area like Mineralogy,
- Ferric, Ferrous, Aqueous solution and Magnetite most often made with reference to Redox.
Hiroshi Ohmoto has researched Sedimentary rock in several fields, including Volcano, Volcanic rock, δ34S, Sulfate and Isotope fractionation.
His studies deal with areas such as Precambrian and Biosphere as well as Archean.
Within one scientific family, Hiroshi Ohmoto focuses on topics pertaining to Organic matter under Sulfur, and may sometimes address concerns connected to Inorganic chemistry, Hydrothermal circulation, Submarine, Deep sea and Abiotic component.
Between 2004 and 2021, his most popular works were:
- Sulphur isotope evidence for an oxic Archaean atmosphere (186 citations)
- Anomalous Fractionations of Sulfur Isotopes During Thermochemical Sulfate Reduction (113 citations)
- Rare earth elements in Precambrian banded iron formations: Secular changes of Ce and Eu anomalies and evolution of atmospheric oxygen (76 citations)
In his most recent research, the most cited papers focused on:
- Mineral
- Carbon dioxide
- Sedimentary rock
Hiroshi Ohmoto mostly deals with Geochemistry, Earth science, Paleontology, Isotope fractionation and Precambrian.
His research on Geochemistry frequently links to adjacent areas such as Mineralogy.
The Mineralogy study combines topics in areas such as Chlorite and Sericite.
His work on Geologic record, Clastic rock and Diagenesis as part of general Paleontology study is frequently linked to Paleoatmosphere, therefore connecting diverse disciplines of science.
His research investigates the link between Geologic record and topics such as Sedimentary rock that cross with problems in Sulfur, Inorganic chemistry and Organic matter.
His work deals with themes such as Solvent models, Solvation and Analytical chemistry, which intersect with Isotope fractionation.
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