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 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.
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.
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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Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation
Max W. Schmidt;Stefano Poli.
Earth and Planetary Science Letters (1998)
Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al-in-hornblende barometer
Max W. Schmidt.
Contributions to Mineralogy and Petrology (1992)
Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth
Ronit Kessel;Max W. Schmidt;Peter Ulmer;Thomas Pettke.
Petrology of subducted slabs
Stefano Poli;Max W. Schmidt.
Annual Review of Earth and Planetary Sciences (2002)
H2O transport and release in subduction zones : experimental constraints on basaltic and andesitic systems
Stefano Poli;Max W. Schmidt.
Journal of Geophysical Research (1995)
Melting and dissolution of subducting crust at high pressures: the key role of white mica
Max W. Schmidt;Daniel Vielzeuf;Estelle Auzanneau.
Earth and Planetary Science Letters (2004)
Melting relations in hydrous systems revisited: application to metapelites, metagreywackes and metabasalts
D. Vielzeuf;M. W. Schmidt.
Contributions to Mineralogy and Petrology (2001)
Redox freezing and melting in the Earth/'s deep mantle resulting from carbon-iron redox coupling
Arno Rohrbach;Max W. Schmidt.
The water–basalt system at 4 to 6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700 to 1400 °C
R. Kessel;P. Ulmer;Thomas Pettke;M.W. Schmidt.
Earth and Planetary Science Letters (2005)
Experimental determination of trace element partitioning between garnet and silica‐rich liquid during anhydrous partial melting of MORB‐like eclogite
M. Pertermann;M. Pertermann;M. M. Hirschmann;K. Hametner;D. Günther.
Geochemistry Geophysics Geosystems (2004)
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