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An Event-Based Depositional Model for the Paleocene–Eocene Sandy–Clayey–Siliceous Sequence of the Russian Platform
© 2018, Pleiades Publishing, Ltd. An event-based depositional model for the Paleocene—Eocene sandy–clayey–siliceous

ESR and spin-lattice relaxation of Nd3+ in silicates of various structures-lattice relaxation gives the positions of the nearest excited Stark level of Nd3+ in the silicates. © 1983 Plenum

PLA synthesis and photocatalytic properties of bismuth silicatesIn this work, bismuth silicates were obtained by pulsed laser ablation in a liquid (PLA).

The molecular dynamics of silica acids in aqueous solution: Qualitative and quantitative characteristics of oligomers of silicic acid oligomers with Sin=(3−8) obtained during molecular dynamics in a reaction Feston

Direct observation of «cholesterol - Model of biological membrane» complex by NMR spectroscopyInteraction and aggregation of cholesterol and sodium dodecyl sulfate molecules were studied

Clay minerals and detrital material in Paleocene–Eocene biogenic siliceous rocks (Sw western Siberia): Implications for volcanic and depositional environment recordClay minerals and detrital material in Paleocene–Eocene biogenic siliceous rocks (Sw western

Silicates of alkaline-earth elements activated RRe-ions – promising materials for scintillation and luminescences applicationsSilicates of alkaline-earth elements activated RRe-ions – promising materials for scintillation

ICP-AES Silicate Analysis of Geological and Technical Materials with Concentration Ratio CalibrationIn solving the problem of improving the accuracy of the ICP-AES procedures for silicate analysis

Formation of coloring complexes in glass colored with cerium and titanium oxides-titanium complexes formed in silicate glass was analyzed. It was found that an active separate reaction between

Variability in distribution of major and trace elements in Lower Eocene siliceous sections of the Transuralian Region, Russia
formation siliceous rocks (Transuralian Region) outcropping in a quarry in the Irbit deposit (thickness

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