What is he best known for?
The fields of study he is best known for:
- Mineral
- Igneous rock
- Hydrogen
His primary areas of study are Geochemistry, Mineralogy, Solidus, Mantle wedge and Peridotite.
His biological study spans a wide range of topics, including Phengite, Partial melting, Outer core, Analytical chemistry and Mechanics.
His work investigates the relationship between Solidus and topics such as Coesite that intersect with problems in Carbonate.
His Mantle wedge study combines topics in areas such as Volcanic arc, Mantle and Subduction zone metamorphism.
His Mantle research includes elements of Planetary differentiation and Petrology.
His Peridotite research incorporates elements of Slab and Lawsonite.
His most cited work include:
- Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation (1389 citations)
- Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al-in-hornblende barometer (956 citations)
- Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth (860 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of investigation include Geochemistry, Mineralogy, Mantle, Analytical chemistry and Silicate.
His Mineralogy research integrates issues from Eutectic system, Partial melting, Kyanite, Thermodynamics and Solidus.
His work carried out in the field of Mantle brings together such families of science as Mantle wedge, Olivine, Carbonate, Transition zone and Oceanic crust.
The various areas that Max W. Schmidt examines in his Analytical chemistry study include Partition coefficient, Crystallization, Diamond, Fractionation and Rutile.
His Silicate study incorporates themes from Metal and Mineral.
His Crust research includes themes of Basalt, Petrology and Amphibole.
He most often published in these fields:
- Geochemistry (36.87%)
- Mineralogy (31.84%)
- Mantle (25.14%)
What were the highlights of his more recent work (between 2015-2021)?
- Geochemistry (36.87%)
- Fractionation (8.38%)
- Mantle (25.14%)
In recent papers he was focusing on the following fields of study:
Max W. Schmidt focuses on Geochemistry, Fractionation, Mantle, Carbonatite and Analytical chemistry.
His study ties his expertise on Volcanic arc together with the subject of Geochemistry.
While the research belongs to areas of Volcanic arc, Max W. Schmidt spends his time largely on the problem of Slab, intersecting his research to questions surrounding Metasomatism.
Max W. Schmidt interconnects Mantle wedge and Olivine in the investigation of issues within Mantle.
His Analytical chemistry research is multidisciplinary, incorporating perspectives in Partition coefficient, Pyroxene and Silicate.
The Graphite study combines topics in areas such as Diamond and Mineralogy.
Between 2015 and 2021, his most popular works were:
- The global systematics of primitive arc melts (55 citations)
- Asthenospheric kimberlites: Volatile contents and bulk compositions at 7 GPa (34 citations)
- A common origin of carbonatite magmas (28 citations)
In his most recent research, the most cited papers focused on:
- Mineral
- Igneous rock
- Hydrogen
Max W. Schmidt mainly investigates Geochemistry, Carbonatite, Mantle, Nitrogen and Earth.
His Geochemistry study frequently links to related topics such as Volcanic arc.
His Nephelinite study, which is part of a larger body of work in Carbonatite, is frequently linked to Cape verde, bridging the gap between disciplines.
His Mantle research is multidisciplinary, incorporating elements of Slab, Basalt, Diamond and Mantle wedge.
His biological study deals with issues like Silicate, which deal with fields such as Calcite, Fractionation, Apatite and Peralkaline rock.
His Accretion research focuses on Analytical chemistry and how it connects with Olivine, Pyroxene, Peridotite and Kimberlite.
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