What is she best known for?
The fields of study she is best known for:
- Volcano
- Basalt
- Plate tectonics
Katherine A. Kelley mainly investigates Mantle, Subduction, Geochemistry, Basalt and Mineralogy.
Katherine A. Kelley specializes in Mantle, namely Mineral redox buffer.
Her Geochemistry study deals with Volcanic arc intersecting with Seamount, Forearc, Lile, Lithophile and Volcano.
Katherine A. Kelley has included themes like Trace element and Pacific Plate in her Basalt study.
Her study looks at the relationship between Mineralogy and fields such as Back-arc basin, as well as how they intersect with chemical problems.
Her biological study spans a wide range of topics, including Adakite and Mantle wedge.
Her most cited work include:
- Water and the Oxidation State of Subduction Zone Magmas (454 citations)
- Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system (420 citations)
- Composition of altered oceanic crust at ODP Sites 801 and 1149 (379 citations)
What are the main themes of her work throughout her whole career to date?
Katherine A. Kelley mostly deals with Geochemistry, Mantle, Subduction, Basalt and Petrology.
Katherine A. Kelley works mostly in the field of Geochemistry, limiting it down to concerns involving Forearc and, occasionally, Rift.
Her Mantle study incorporates themes from Ridge, Volcanic arc, Mantle wedge and Oceanic crust.
Her Subduction research focuses on Earth science and how it connects with Flux melting.
Her research on Basalt also deals with topics like
- Mineralogy which connect with Back-arc basin and Silicate,
- Igneous rock which connect with Waves and shallow water.
In her research on the topic of Petrology, Seamount is strongly related with Volcano.
She most often published in these fields:
- Geochemistry (56.25%)
- Mantle (43.75%)
- Subduction (36.81%)
What were the highlights of her more recent work (between 2016-2021)?
- Geochemistry (56.25%)
- Basalt (30.56%)
- Mineral redox buffer (13.89%)
In recent papers she was focusing on the following fields of study:
Katherine A. Kelley spends much of her time researching Geochemistry, Basalt, Mineral redox buffer, Volcanology and Mantle.
Her work on Mid-ocean ridge and Igneous differentiation as part of her general Geochemistry study is frequently connected to Descent and Oxidizing agent, thereby bridging the divide between different branches of science.
The concepts of her Basalt study are interwoven with issues in Mineral physics and Analytical chemistry.
Magnetite, Sulfide, Forearc and Flux melting is closely connected to Trace element in her research, which is encompassed under the umbrella topic of Mineral redox buffer.
Her Volcanology research incorporates elements of Subduction and Petrology.
Her research in Mantle intersects with topics in Ridge and Mantle wedge.
Between 2016 and 2021, her most popular works were:
- Heterogeneity in mantle carbon content from CO 2 -undersaturated basalts. (53 citations)
- Determination of Fe3+/ΣFe of XANES basaltic glass standards by Mössbauer spectroscopy and its application to the oxidation state of iron in MORB (43 citations)
- Interplay of crystal fractionation, sulfide saturation and oxygen fugacity on the iron isotope composition of arc lavas: An example from the Marianas (26 citations)
In her most recent research, the most cited papers focused on:
- Basalt
- Volcano
- Plate tectonics
Her primary areas of study are Basalt, Mineral redox buffer, Geochemistry, Mantle and Analytical chemistry.
Her specific area of interest is Basalt, where Katherine A. Kelley studies Melt inclusions.
In her study, Magnetite, Sulfide, Forearc and Flux melting is inextricably linked to Trace element, which falls within the broad field of Mineral redox buffer.
Her research integrates issues of Silicate and Isotopes of potassium in her study of Geochemistry.
Her research in Mantle tackles topics such as Ridge which are related to areas like Vulcanian eruption.
Her study in Peridotite is interdisciplinary in nature, drawing from both Subduction, Mantle wedge and Earth science.
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