What is he best known for?
The fields of study he is best known for:
- Igneous rock
- Basalt
- Geochemistry
The scientist’s investigation covers issues in Geochemistry, Archean, Tonalite-Trondhjemite-Granodiorite, Adakite and Sanukitoid.
In the field of Geochemistry, his study on Partial melting, Mantle, Fractional crystallization and Crust overlaps with subjects such as Population.
The study incorporates disciplines such as Felsic and Basalt in addition to Mantle.
The concepts of his Archean study are interwoven with issues in Plate tectonics, Continental crust and Petrogenesis.
In his research, Dharwar Craton and Subduction is intimately related to Petrology, which falls under the overarching field of Continental crust.
Jean-François Moyen works mostly in the field of Tonalite-Trondhjemite-Granodiorite, limiting it down to concerns involving Eclogite and, occasionally, Paleoarchean and Mafic.
His most cited work include:
- An overview of adakite, tonalite–trondhjemite–granodiorite (TTG), and sanukitoid: relationships and some implications for crustal evolution (1709 citations)
- High Sr/Y and La/Yb ratios: The meaning of the “adakitic signature” (577 citations)
- Forty years of TTG research (447 citations)
What are the main themes of his work throughout his whole career to date?
Geochemistry, Archean, Continental crust, Crust and Petrology are his primary areas of study.
His work carried out in the field of Geochemistry brings together such families of science as Craton and Pluton.
Jean-François Moyen has researched Archean in several fields, including Tectonics, Plate tectonics, Petrogenesis, Paleoarchean and Mafic.
He has researched Petrogenesis in several fields, including Tonalite-Trondhjemite-Granodiorite and Eclogite.
Within one scientific family, Jean-François Moyen focuses on topics pertaining to Subduction under Continental crust, and may sometimes address concerns connected to Geothermal gradient.
His Mantle research incorporates elements of Sanukitoid and Mantle wedge.
He most often published in these fields:
- Geochemistry (104.27%)
- Archean (52.99%)
- Continental crust (30.77%)
What were the highlights of his more recent work (between 2018-2021)?
- Geochemistry (104.27%)
- Archean (52.99%)
- Zircon (19.66%)
In recent papers he was focusing on the following fields of study:
Jean-François Moyen mainly investigates Geochemistry, Archean, Zircon, Batholith and Continental crust.
His Geochemistry study deals with Pluton intersecting with Craton.
Jean-François Moyen has included themes like Tectonics and Early Earth in his Archean study.
His Zircon research also works with subjects such as
- Geochronology together with Terrane, Pilbara Craton, Petrology and Petrogenesis,
- Thermochronology, Recrystallization, Protolith, Migmatite and Igneous rock most often made with reference to Anatexis,
- Partial melting and related Radiometric dating.
His work investigates the relationship between Batholith and topics such as Dharwar Craton that intersect with problems in Trace element, Mantle and Titanite.
He combines subjects such as Cadomian Orogeny and Earth crust with his study of Continental crust.
Between 2018 and 2021, his most popular works were:
- Earth’s earliest granitoids are crystal-rich magma reservoirs tapped by silicic eruptions (31 citations)
- Detrital zircon U-Pb-Hf systematics of Ediacaran metasediments from the French Massif Central: Consequences for the crustal evolution of the north Gondwana margin (12 citations)
- Chemical variation, modal composition and classification of granitoids (11 citations)
In his most recent research, the most cited papers focused on:
- Igneous rock
- Basalt
- Geochemistry
Jean-François Moyen mainly focuses on Geochemistry, Phase equilibrium, Continental crust, Composition and Archean.
His Geochemistry research integrates issues from Gondwana and Current.
Phase equilibrium combines with fields such as Mass transfer and Process oriented in his investigation.
Jean-François Moyen interconnects Felsic, Basalt, Silicic, Phenocryst and Pluton in the investigation of issues within Continental crust.
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