2022 - Research.com Earth Science in Russia Leader Award
Konstantin D. Litasov spends much of his time researching Mineralogy, Mantle, Analytical chemistry, Transition zone and Peridotite. His Mineralogy study combines topics from a wide range of disciplines, such as Diamond anvil cell, Hydrogen, Diamond and Stishovite. His Ringwoodite study in the realm of Mantle interacts with subjects such as Solidus.
His biological study spans a wide range of topics, including Periclase, Bulk modulus, Pyrophyllite and Olivine. His study in Peridotite is interdisciplinary in nature, drawing from both Subduction, Igneous rock and Partial melting. Konstantin D. Litasov has included themes like Flux melting, Phase and Forsterite in his Partial melting study.
His primary areas of study are Analytical chemistry, Mineralogy, Geochemistry, Mantle and Thermodynamics. His research integrates issues of Carbonate, Phase, Liquidus and Eutectic system in his study of Analytical chemistry. In the field of Mineralogy, his study on Olivine, Wadsleyite and Ringwoodite overlaps with subjects such as Solidus.
Konstantin D. Litasov combines subjects such as Diamond, Eclogite, Petrology and Transition zone with his study of Mantle. His work carried out in the field of Transition zone brings together such families of science as Mantle wedge and Oceanic crust. In general Thermodynamics, his work in Phase transition, Thermal expansion and Bulk modulus is often linked to Earth linking many areas of study.
Konstantin D. Litasov mostly deals with Analytical chemistry, Geochemistry, Phase, Carbonate and Eutectic system. His Analytical chemistry research is multidisciplinary, relying on both Magnesite, Crystallization, Meteorite and Liquidus. His studies in Magnesite integrate themes in fields like Carbonatite and Mantle.
In his research on the topic of Geochemistry, Olivine is strongly related with Silicate. He has researched Carbonate in several fields, including Diamond and Kimberlite. His Eutectic system study integrates concerns from other disciplines, such as Wadsleyite and Aragonite.
His primary scientific interests are in Analytical chemistry, Geochemistry, Eutectic system, Solid solution and Magnesite. His Analytical chemistry research includes themes of Diamond, Parent body, Carbonate, Phase and Meteorite. His Geochemistry research integrates issues from Chromitite and Aluminosilicate.
His Mantle research extends to the thematically linked field of Eutectic system. His Mantle study combines topics in areas such as Lava, Basalt and Dissolution. His studies deal with areas such as Carbonatite and Liquidus as well as Magnesite.
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.
Water transport into the deep mantle and formation of a hydrous transition zone
Eiji Ohtani;Konstantin Litasov;Tomofumi Hosoya;Tomoaki Kubo.
Physics of the Earth and Planetary Interiors (2004)
Phase relations and melt compositions in CMAS-pyrolite-H2O system up to 25 GPa
Konstantin Litasov;Eiji Ohtani.
Physics of the Earth and Planetary Interiors (2002)
Solidus of alkaline carbonatite in the deep mantle
Konstantin D. Litasov;Anton Shatskiy;Eiji Ohtani;Gregory M. Yaxley.
Water solubility in Mg-perovskites and water storage capacity in the lower mantle
Konstantin Litasov;Eiji Ohtani;Falko Langenhorst;Hisayoshi Yurimoto.
Earth and Planetary Science Letters (2003)
Phase relations in hydrous MORB at 18-28 GPa: implications for heterogeneity of the lower mantle
Konstantin D. Litasov;Eiji Ohtani.
Physics of the Earth and Planetary Interiors (2005)
Stability of dense hydrous magnesium silicate phases and water storage capacity in the transition zone and lower mantle
E. Ohtani;M. Toma;K. Litasov;Tomoaki Kubo.
Physics of the Earth and Planetary Interiors (2001)
An Experimental Study of Carbonated Eclogite at 3·5–5·5 GPa—Implications for Silicate and Carbonate Metasomatism in the Cratonic Mantle
Ekaterina S. Kiseeva;Gregory M. Yaxley;Jörg Hermann;Konstantin D. Litasov;Konstantin D. Litasov.
Journal of Petrology (2012)
Solidus of carbonated peridotite from 10 to 20 GPa and origin of magnesiocarbonatite melt in the Earth's deep mantle
Sujoy Ghosh;Eiji Ohtani;Konstantin D. Litasov;Hidenori Terasaki.
Chemical Geology (2009)
The solidus of carbonated eclogite in the system CaO–Al2O3–MgO–SiO2–Na2O–CO2 to 32GPa and carbonatite liquid in the deep mantle
Konstantin Litasov;Eiji Ohtani.
Earth and Planetary Science Letters (2010)
Stability of various hydrous phases in CMAS pyrolite-H 2 O system up to 25 GPa
K. Litasov;E. Ohtani.
Physics and Chemistry of Minerals (2003)
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