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Early Palaeoproterozoic granulite-facies metamorphism and partial melting of eclogite-facies rocks in the Salma association, eastern Fennoscandian Shield, Russia
Dokukina K., Mints M.V., Khubanov V.B., Sheshukov V.S., Konilov A.N., Bayanova T.B., Kaulina T.V., Golunova M.A., Dokukin P.A., Okina O.I., Van K.V., Yudin D.S., Travin A.V., Zaitsev A.V., Kosorukov V.L., Pozhilenko V.I., Golovanova T.I.
at temperatures up to 900 °C and pressure down to 9 kbar, eclogite facies metasediments underwent partial melting
Impact response and dynamic strength of partially melted aluminum alloy
Zaretsky, E. B., Kanel, Gennady I.
Impact response and dynamic strength of partially melted aluminum alloy
Interaction between gaseous oxygen and germanium melt
Shimanskii, A. F., Podkopaev, O. I., Pogodaev, A. M.
Interaction between the residual gaseous oxygen and germanium melt is analyzed. There is a
Effect of Cu and Zr additions on the superplastic behavior of 6061 aluminum alloy
Kaibyshev R., Gromov D., Nieh T.G., Lesuer D.R.
partial melting
ESR evidence for partial melting of the orbital order in LaMnO3 below the Jahn-Teller transition
Schaile S., Von Nidda H., Deisenhofer J., Eremin M., Tokura Y., Loidl A.
distortions. Our results support a partial melting of the orbital order along the antiferromagnetically
Neoarchean high-pressure granulite-facies anatexis of continental rocks in the Belomorian Eclogite Province, Russia
Dokukina K.A., Khiller V.V., Khubanov V.B., Mints M.V., Dokukin P.A., Natapov L., Belousova E., Yakushik M.A.
lithologies, which are the most suitable place for partial melting, fluid migration, and component diffusion
ESR evidence for partial melting of the orbital order in LaMnO3 below the Jahn-Teller transition
Schaile S., Von Nidda H., Deisenhofer J., Eremin M., Tokura Y., Loidl A.
distortions. Our results support a partial melting of the orbital order along the antiferromagnetically
PALEOGEODYNAMICS OF MAGMATIC AND METAMORPHIC PROCESSES OF FORMATION OF ULTRAMAFIC ROCKS OF CHAGAN-UZUN MASSIF (OPHIOLITES OF GORNY ALTAI)
Simonov V.A., Kulikova A.V., Kotlyarov A.V., Kolotilina T.B.
are restites with a degree of partial melting 15-20 %, which formed at temperatures 1520-1420 °С under
The Olivinite of the Krestovskaya Intrusion—the Product of Larnite-Normative Alkali Ultramafic Magma: Melt Inclusion Data
Сазонов, Анатолий Максимович, Panina, L. I., Isakova, A. T.
distribution, and geochemical indicator ratios evidenced that the magma was derived by the partial melting
Natural convection melting influence on the thermal resistance of a brick partially filled with phase change material
Bondareva, Nadezhda S., Sheremet, Mikhail A.
material. Heat transfer, taking into account melting in brick, was analyzed at various temperature

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