Maxim Portnyagin mainly focuses on Geochemistry, Melt inclusions, Mantle, Mantle wedge and Olivine. His study in Geochemistry focuses on Fractional crystallization, Basalt, Volcano and Magma. The various areas that he examines in his Mantle study include Slab, Subduction, Volcanic arc and Transition zone.
The study incorporates disciplines such as Mantle plume and Ultramafic rock in addition to Transition zone. His Mantle wedge research incorporates themes from Adakite, Oceanic crust and Peridotite. Olivine is closely attributed to Phenocryst in his work.
Maxim Portnyagin mainly investigates Geochemistry, Volcano, Melt inclusions, Olivine and Basalt. His Geochemistry research is multidisciplinary, incorporating elements of Subduction and Earth science. While the research belongs to areas of Melt inclusions, he spends his time largely on the problem of Petrology, intersecting his research to questions surrounding Lava.
His studies deal with areas such as Mantle plume, Mineral redox buffer, Crust and Analytical chemistry as well as Olivine. His study in Basalt is interdisciplinary in nature, drawing from both Island arc and Volcanic rock. As a part of the same scientific family, Maxim Portnyagin mostly works in the field of Mantle, focusing on Mantle wedge and, on occasion, Adakite.
His primary areas of study are Geochemistry, Volcano, Olivine, Mantle and Tephra. His Geochemistry study frequently draws connections between adjacent fields such as Oceanic crust. He combines subjects such as Sedimentary rock and Pleistocene with his study of Volcano.
His work in the fields of Melt inclusions overlaps with other areas such as Silicate. His study on Melt inclusions also encompasses disciplines like
Maxim Portnyagin mostly deals with Mantle, Olivine, Melt inclusions, Petrology and Crust. Mantle is closely attributed to Basalt in his research. The various areas that Maxim Portnyagin examines in his Basalt study include Electron microprobe, Microanalysis, Analytical chemistry and Breccia.
His Melt inclusions study frequently involves adjacent topics like Continental crust. His work carried out in the field of Petrology brings together such families of science as Mineral redox buffer, Mantle wedge and Island arc. Crust is a subfield of Geochemistry that Maxim Portnyagin investigates.
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Constraints on mantle melting and composition and nature of slab components in volcanic arcs from volatiles (H 2 O, S, Cl, F) and trace elements in melt inclusions from the Kamchatka Arc
Maxim Portnyagin;Kaj Hoernle;Pavel Plechov;Nikita Mironov.
Earth and Planetary Science Letters (2007)
Oxygen isotope evidence for slab melting in modern and ancient subduction zones
I. N. Bindeman;I. N. Bindeman;J. M. Eiler;G. M. Yogodzinski;Y. Tatsumi.
Earth and Planetary Science Letters (2005)
Experimental evidence for rapid water exchange between melt inclusions in olivine and host magma
Maxim Portnyagin;Renat Almeev;Sergei Matveev;François Holtz.
Earth and Planetary Science Letters (2008)
Solubility of H2O- and CO2-bearing fluids in tholeiitic basalts at pressures up to 500 MPa
T. A. Shishkina;R. E. Botcharnikov;F. Holtz;R. R. Almeev.
Chemical Geology (2010)
Subduction cycling of volatiles and trace elements through the Central American volcanic arc: evidence from melt inclusions
Seth J. Sadofsky;Maxim Portnyagin;Kaj Hoernle;Kaj Hoernle;Paul van den Bogaard;Paul van den Bogaard.
Contributions to Mineralogy and Petrology (2008)
Komatiites reveal a hydrous Archaean deep-mantle reservoir
Alexander V. Sobolev;Evgeny V. Asafov;Andrey A. Gurenko;Nicholas T. Arndt.
The origin of hydrous, high-δ18O voluminous volcanism: diverse oxygen isotope values and high magmatic water contents within the volcanic record of Klyuchevskoy volcano, Kamchatka, Russia
Sara Auer;Ilya Bindeman;Paul Wallace;Vera Ponomareva.
Contributions to Mineralogy and Petrology (2009)
Large-volume silicic volcanism in Kamchatka: Ar-Ar and U-Pb ages, isotopic, and geochemical characteristics of major pre-Holocene caldera-forming eruptions
I.N. Bindeman;V.L. Leonov;P.E. Izbekov;V.V. Ponomareva.
Journal of Volcanology and Geothermal Research (2010)
Drastic shift in lava geochemistry in the volcanic-front to rear-arc region of the Southern Kamchatkan subduction zone: Evidence for the transition from slab surface dehydration to sediment melting
Svend Duggen;Maxim Portnyagin;Maxim Portnyagin;Joel Baker;David Ulfbeck.
Geochimica et Cosmochimica Acta (2007)
Geochemistry of primitive lavas of the Central Kamchatka Depression: magma generation at the edge of the Pacific plate
Maxim Portnyagin;Ilya Bindeman;Kaj Hoernle;Folkmar Hauff.
Geophysical monograph (2007)
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