What is he best known for?
The fields of study he is best known for:
- Mineral
- Thermodynamics
- Composite material
John D. Fitz Gerald spends much of his time researching Mineralogy, Grain boundary, Grain size, Transmission electron microscopy and Condensed matter physics.
His work carried out in the field of Mineralogy brings together such families of science as Mica, Metasomatism, Plagioclase, Mafic and Albite.
The concepts of his Grain boundary study are interwoven with issues in Shear stress, Olivine and Deformation.
As a part of the same scientific study, John D. Fitz Gerald usually deals with the Grain size, concentrating on Grain Boundary Sliding and frequently concerns with Shear modulus.
His research integrates issues of Nucleation, Amorphous solid, Nanostructure, Annealing and Boron nitride in his study of Transmission electron microscopy.
Many of his research projects under Condensed matter physics are closely connected to Attenuation, Glassy carbon, Magnetic hysteresis and Production with Attenuation, Glassy carbon, Magnetic hysteresis and Production, tying the diverse disciplines of science together.
His most cited work include:
- Grain-size-sensitive seismic wave attenuation in polycrystalline olivine (301 citations)
- Unconventional Magnetism in All-Carbon Nanofoam (207 citations)
- Relationships between dynamically recrystallized grain size and deformation conditions in experimentally deformed olivine rocks (204 citations)
What are the main themes of his work throughout his whole career to date?
The scientist’s investigation covers issues in Mineralogy, Crystallography, Grain boundary, Condensed matter physics and Annealing.
His Mineralogy study incorporates themes from Shear modulus, Microstructure, Grain size and Viscoelasticity.
The Crystallography study combines topics in areas such as Transmission electron microscopy and Solid solution.
His biological study spans a wide range of topics, including Wetting, Crystallite and Shear stress.
His study looks at the intersection of Condensed matter physics and topics like Electron diffraction with Ferroelectricity and Reciprocal lattice.
His Annealing study deals with Boron nitride intersecting with Nanostructure and Nanotube.
He most often published in these fields:
- Mineralogy (44.57%)
- Crystallography (17.39%)
- Grain boundary (16.30%)
What were the highlights of his more recent work (between 2008-2016)?
- Mineralogy (44.57%)
- Geochemistry (6.52%)
- Geophysics (6.52%)
In recent papers he was focusing on the following fields of study:
Mineralogy, Geochemistry, Geophysics, Magnetofossil and Magnetotactic bacteria are his primary areas of study.
He merges Mineralogy with Cathodoluminescence in his study.
His Geochemistry research is multidisciplinary, incorporating perspectives in Oxide, Chlorite and Block.
In his research, Seismology is intimately related to Dislocation, which falls under the overarching field of Geophysics.
John D. Fitz Gerald works mostly in the field of Magnetotactic bacteria, limiting it down to topics relating to Anoxic waters and, in certain cases, Carbonate, as a part of the same area of interest.
His Scanning electron microscope study integrates concerns from other disciplines, such as Crystallography, Microstructure, Grain boundary and Transmission electron microscopy.
Between 2008 and 2016, his most popular works were:
- Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron (116 citations)
- Magnetotactic bacterial response to Antarctic dust supply during the Palaeocene-Eocene thermal maximum (53 citations)
- Identification and environmental interpretation of diagenetic and biogenic greigite in sediments: A lesson from the Messinian Black Sea (51 citations)
In his most recent research, the most cited papers focused on:
- Thermodynamics
- Mineral
- Composite material
John D. Fitz Gerald mainly focuses on Magnetofossil, Magnetotactic bacteria, Mineralogy, Paleontology and Diagenesis.
In his study, Sedimentary rock and Carbonate is strongly linked to Anoxic waters, which falls under the umbrella field of Magnetotactic bacteria.
John D. Fitz Gerald integrates Mineralogy and Microscopy in his studies.
His work on Geologic record, Weathering, Magnetosome and Environmental magnetism as part of general Paleontology research is often related to Plateau, thus linking different fields of science.
His Magnetite research is multidisciplinary, relying on both Deep sea, Aeolian processes and Geochemistry.
His study in Geophysics is interdisciplinary in nature, drawing from both Dislocation creep and Dislocation.
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