What is he best known for?
The fields of study he is best known for:
- Thermodynamics
- Basalt
- Igneous rock
His scientific interests lie mostly in Zircon, Geochemistry, Eclogite, Subduction and Coesite.
His Zircon research includes themes of Gneiss, Mineralogy and Petrology.
His Mineralogy study combines topics from a wide range of disciplines, such as Deformation, Fugacity and Geophysics.
Specifically, his work in Geochemistry is concerned with the study of Mantle.
His Subduction study combines topics in areas such as Olivine, Seismic anisotropy and Continental crust.
His Coesite research integrates issues from Metamorphism and Ultramafic rock.
His most cited work include:
- Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies (465 citations)
- Global UHP metamorphism and continental subduction/collision: The himalayan model (303 citations)
- Global UHP metamorphism and continental subduction/collision: The himalayan model (303 citations)
What are the main themes of his work throughout his whole career to date?
Ikuo Katayama spends much of his time researching Geochemistry, Petrology, Mineralogy, Subduction and Mantle.
His Geochemistry study frequently draws connections to adjacent fields such as Eclogite.
His Petrology research is multidisciplinary, incorporating perspectives in Permeability, Dilatant and Peridotite.
His Subduction research is multidisciplinary, incorporating elements of Geophysics and Continental crust.
His research integrates issues of Ophiolite, Basalt, Oceanic crust and Crust in his study of Mantle.
His work in Zircon addresses issues such as Coesite, which are connected to fields such as Terrane and Kyanite.
He most often published in these fields:
- Geochemistry (33.00%)
- Petrology (28.57%)
- Mineralogy (18.72%)
What were the highlights of his more recent work (between 2015-2021)?
- Petrology (28.57%)
- Composite material (9.85%)
- Deformation (7.39%)
In recent papers he was focusing on the following fields of study:
Petrology, Composite material, Deformation, Mantle and Geotechnical engineering are his primary areas of study.
His Mafic study, which is part of a larger body of work in Petrology, is frequently linked to Volcanology, bridging the gap between disciplines.
He interconnects Subduction, Oceanic crust and Crust in the investigation of issues within Mantle.
Ikuo Katayama combines subjects such as Slab and Fault with his study of Subduction.
Ikuo Katayama is conducting research in Geochemistry and Mineralogy as part of his Clay minerals study.
In his works, Ikuo Katayama undertakes multidisciplinary study on Geochemistry and Dehydration.
Between 2015 and 2021, his most popular works were:
- Mantle hydration along outer-rise faults inferred from serpentinite permeability. (12 citations)
- What is the origin of macroscopic friction (10 citations)
- Effects of humidity and interlayer cations on the frictional strength of montmorillonite (10 citations)
In his most recent research, the most cited papers focused on:
- Thermodynamics
- Basalt
- Igneous rock
The scientist’s investigation covers issues in Deformation, Petrology, Composite material, Subduction and Pore water pressure.
His study on Deformation also encompasses disciplines like
- Dilatant and related Mafic, Peridotite and Gabbro,
- Geotechnical engineering which is related to area like Rheology and Strain.
His biological study deals with issues like Porosity, which deal with fields such as Core, Seismic refraction and Seismic velocity.
His work on Montmorillonite as part of general Composite material study is frequently connected to Brucite, therefore bridging the gap between diverse disciplines of science and establishing a new relationship between them.
His studies in Subduction integrate themes in fields like Slab, Fault, Transition zone and Mantle.
His Mantle research focuses on Oceanic crust and how it relates to Mohorovičić discontinuity, Earth science, Crust and Seafloor spreading.
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