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Middle Paleoproterozoic active continental margin of Sarmatia

Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.

Northeastern part of the Archean Sarmatia continent

Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.

Neoarchean Volgo-Uralia continent

Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.

Petrologic research techniques

Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.

Late Paleoproterozoic late- and postcollisional granitoid and alkaline magmatism

Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.

Late Paleoproterozoic Svecofennian accretionary orogen

Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.

Heavy metals in marine aerosols of the AZOV sea

Chichaeva M.A., Lychagin M.Y., Syroeshkin A.V., Chernitsova O.V.

. The ranges of contents were determined as following: Fe (200 – 2000 ng / m3), Al (20 – 200 ng / m3), Zn (10

Neutrophil Activation by Mineral Microparticles Coated with Methylglyoxal-Glycated Albumin

Mikhalchik E.V., Ivanov V.A., Borodina I.V., Borodina O.V., Smirnov I.P., Gorudko I.V., Grigorieva D.V., Boychenko O.P., Moskalets A.P., Klinov D.V., Panasenko O.M., Filatova L.Y., Kirzhanova E.A., Balabushevich N.G.

nanocrystals (vaterite polymorph, CC) or hydroxyapatite nanowires (CP). As scopoletin fluorescence has shown, H

Избранные вопросы современной науки

Grebennikov A.V., Makarova N.G., Menshchikova I.Yu., Prosenko A.E., Казаков М.А., Матвеевская Н.С., Terakh E.I.

Biophysics education section and computational training discussion at VII Congress of Russian Biophysicists

Turkina V.A., Orlova N.G., Orlov Y.L.

. © 2023, International Union for Pure and Applied Biophysics (IUPAB) and Springer-Verlag GmbH Germany

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