What is he best known for?
The fields of study he is best known for:
- Basalt
- Volcano
- Igneous rock
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.
His most cited work include:
- 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 (225 citations)
- Oxygen isotope evidence for slab melting in modern and ancient subduction zones (173 citations)
- Experimental evidence for rapid water exchange between melt inclusions in olivine and host magma (165 citations)
What are the main themes of his work throughout his whole career to date?
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.
He most often published in these fields:
- Geochemistry (83.84%)
- Volcano (34.06%)
- Melt inclusions (37.12%)
What were the highlights of his more recent work (between 2018-2021)?
- Geochemistry (83.84%)
- Volcano (34.06%)
- Olivine (35.81%)
In recent papers he was focusing on the following fields of study:
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
- Crust together with Island arc,
- Petrology which connect with Mineral redox buffer and Mantle wedge.
His work deals with themes such as Explosive eruption, Volcanic arc and Zircon, which intersect with Tephra.
Between 2018 and 2021, his most popular works were:
- Deep hydrous mantle reservoir provides evidence for crustal recycling before 3.3 billion years ago (23 citations)
- Deep hydrous mantle reservoir provides evidence for crustal recycling before 3.3 billion years ago (23 citations)
- New Olivine Reference Material for In Situ Microanalysis (21 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Volcano
- Igneous rock
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.
This overview was generated by a machine learning system which analysed the scientist’s
body of work. If you have any feedback, you can
contact us
here.
