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Early Mesozoic lamproites and monzonitoids of southeastern Gorny Altai: geochemistry, Sr–Nd isotope composition, and sources of melts and the higher degree of its partial melting as compared with the derivates of the Chuya and Tarkhata complexes

The origin of the Palaeoproterozoic AMCG complexes in the Ukrainian shield: New U-Pb ages and Hf isotopes in zircon-derived tholeiitic magma into the lower crust. This resulted in partial melting of mafic lower-crustal material

The Effect of Pulsed Laser Radiation on a Si Layer with a High Dose of Implanted Ag+ Ions impurity partial diffusion within the melted layer, as well as Ag partial evaporation during the PLA.

Particle forming amorphous solid dispersions: A mechanistic randomized pharmacokinetic study in humans essential insights into underlying mechanisms of ASD functioning in humans, partially validating current

Heat transfer performance of the finned nano-enhanced phase change material system under the inclination influence to store and transport the heat. The intensity of melting is related to the thermophysical characteristics

Parental sources of high-alumina alkaline melts: Nd, Sr, Pb, and O isotopic evidence from the Devonian Kiya-Shaltyr gabbro-urtite intrusion, South Siberia place under conditions of partial mingling of matter of the depleted (PREMA) and enriched (EM) mantle

The effect of hot wall configuration on melting flow of nano-enhanced phase change material inside a tilted square capsulePCM). The porosity-enthalpy technique is used to track the melting flow. The correctness of the obtained numerical

Deposition and characterization of alumina-titania coating by multi-chamber gas-dynamic sprayer. The results show that the alumina-titania coatings consist of both fully melted regions and partially melted

Magnetic susceptibility of CoFeBSiNb alloys in liquid state of the Slovak Academic Information Agency. The work is partially supported by RFBR, project N 13-03-00598-a.

Magnetic susceptibility of CoFeBSiNb alloys in liquid state of the Slovak Academic Information Agency. The work is partially supported by RFBR, project N 13-03-00598-a.

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