What is he best known for?
The fields of study he is best known for:
- Igneous rock
- Basalt
- Magma
His primary scientific interests are in Mineralogy, Amphibole, Analytical chemistry, Olivine and Geochemistry.
His work on Electron microprobe as part of general Mineralogy study is frequently linked to Partition coefficient, bridging the gap between disciplines.
His research integrates issues of Andesite, Basaltic andesite and Partial melting in his study of Analytical chemistry.
His work focuses on many connections between Olivine and other disciplines, such as Peridotite, that overlap with his field of interest in Basanite, Polybaric melting, Majorite and Transition zone.
His biological study focuses on Pyroxene.
His Pyroxene research includes elements of Metasomatism and Mantle.
His most cited work include:
- Experimental studies of trace-element partitioning applicable to igneous petrogenesis — Sedona 16 years later (504 citations)
- Genesis of the calc-alkaline igneous rock suite (496 citations)
- Genesis of the calc-alkaline igneous rock suite (496 citations)
What are the main themes of his work throughout his whole career to date?
Trevor H. Green mostly deals with Mineralogy, Geochemistry, Analytical chemistry, Partition coefficient and Amphibole.
His Mineralogy research integrates issues from Andesite, Basaltic andesite and Trace element.
His Geochemistry study combines topics in areas such as Plagioclase and Phenocryst.
His Analytical chemistry research focuses on subjects like Mineral redox buffer, which are linked to Crystal.
His work carried out in the field of Amphibole brings together such families of science as Lile, Partial melting and Olivine, Mantle minerals.
His Olivine research is multidisciplinary, relying on both Basanite and Peridotite.
He most often published in these fields:
- Mineralogy (60.00%)
- Geochemistry (45.71%)
- Analytical chemistry (35.71%)
What were the highlights of his more recent work (between 1999-2019)?
- Trace element (25.71%)
- Mineralogy (60.00%)
- Geochemistry (45.71%)
In recent papers he was focusing on the following fields of study:
His main research concerns Trace element, Mineralogy, Geochemistry, Basalt and Amphibole.
His Trace element research is multidisciplinary, incorporating perspectives in Mafic, Mantle wedge and Omphacite.
Trevor H. Green has researched Mineralogy in several fields, including Basanite and Analytical chemistry.
His study in the field of Mantle and Apatite also crosses realms of Partition coefficient, Minor and Solubility.
In the subject of general Basalt, his work in Partial melting is often linked to Intraplate earthquake, thereby combining diverse domains of study.
His study in Amphibole is interdisciplinary in nature, drawing from both Phenocryst, Igneous differentiation and Peridotite.
Between 1999 and 2019, his most popular works were:
- SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C (433 citations)
- Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis (416 citations)
- Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt : 1. Experimental results and the investigation of controls on partitioning behaviour (403 citations)
In his most recent research, the most cited papers focused on:
- Igneous rock
- Basalt
- Magma
His scientific interests lie mostly in Mineralogy, Trace element, Analytical chemistry, Basalt and Amphibole.
His Trace element study incorporates themes from Metasomatism, Mantle wedge, Residuum and Omphacite.
His Analytical chemistry study often links to related topics such as Partial melting.
As part of one scientific family, Trevor H. Green deals mainly with the area of Basalt, narrowing it down to issues related to the Oceanic crust, and often Eclogite.
His work deals with themes such as Geochemistry, Mantle and Pyroxene, which intersect with Eclogite.
His work in Amphibole addresses subjects such as Basanite, which are connected to disciplines such as Peridotite and Olivine.
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