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.
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.
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
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.
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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Isotopes of sulfur and carbon
Geochemistry of Hydrothermal Ore Deposits (1979)
SYSTEMATICS OF SULFUR AND CARBON ISOTOPES IN HYDROTHERMAL ORE DEPOSITS
Economic Geology (1972)
Stable isotope geochemistry of ore deposits
Reviews in Mineralogy & Geochemistry (1986)
Sulfur and Carbon Isotopes
Geochemistry of Hydrothermal Ore Deposits (1997)
Chemical evolution and mineral deposition in boiling hydrothermal systems
S. E. Drummond;H. Ohmoto.
Economic Geology (1985)
Kinetics of reactions between aqueous sulfates and sulfides in hydrothermal systems
Hiroshi Ohmoto;Antonio C. Lasaga.
Geochimica et Cosmochimica Acta (1982)
Geochemistry of ∼1.9 Ga sedimentary rocks from northeastern Labrador, Canada
Ken-Ichiro Hayashi;Hiroyuki Fujisawa;Heinrich D. Holland;Hiroshi Ohmoto;Hiroshi Ohmoto.
Geochimica et Cosmochimica Acta (1997)
Sulfur and Carbon Isotopes and Ore Genesis: A Review
Robert O. Rye;Hiroshi Ohmoto.
Economic Geology (1974)
Formation of volcanogenic massive sulfide deposits: The Kuroko perspective
Hiroshi Ohmoto;Hiroshi Ohmoto.
Ore Geology Reviews (1996)
Evidence in pre–2.2 Ga paleosols for the early evolution of atmospheric oxygen and terrestrial biota
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