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Last glacial ecology and geoarchaeology of the Central Trans-Ural area: The Sosva River Upper Palaeolithic Complex, western SiberiaQuaternary and geoarchaeology studies from the eastern limits of the Ural Mountains provide

Drug release modification by interpolymer interaction between countercharged types of Eudragit® RL 30D and FS 30D in double-layer films of the carboxylate groups that form the ionic bonds with the quaternary ammonium groups. Moreover, while increasing

Геология четвертичных отложений территории Полесской седловиныGeology of Quaternary Deposits on the Territory of Polesje Saddle

Representatives of the genus Fabaeformiscandona Krstič, 1972 (Crustacea, Ostracoda) from Quaternary deposits of Western Siberia, 1900 from the Quaternary deposits of Western Siberia. The main goal is to reassess their generic

Reduction of quaternary salts of 3-azafluorene and 3-azafluorenone and their conversion to indenoindolizines. Indenoindolizines with linear and angular structures were synthesized from the N-phenacyl quaternary salts of 3

The quaternary mammals from Kozhamzhar locality (Pavlodar region, Kazakhstan). The article provides the description of the quaternary sediments section found in the outcrop near Kozhamzhar

Synthesis of Chromenoimidazoles, Annulated with an Azaindole Moiety, through a Base-Promoted Domino Reaction of Cyano methyl Quaternary SaltsThe reactivity of N -cyanomethyl quaternary salts of 4-, 5- and 7-azaindoles towards salicylic

Synthesis and biological activity of quaternary phosphonium salts based on 3-hydroxypyridine and 4-deoxypyridoxine© 2016, Springer Science+Business Media New York.Methods for the synthesis of quaternary

Synthesis and Antibacterial Activity of Quaternary Ammonium 4-Deoxypyridoxine Derivatives© 2016 Nikita V. Shtyrlin et al.A series of novel quaternary ammonium 4-deoxypyridoxine derivatives

Paleosecular Variations of the Geomagnetic Field Isolated in Pliocene–Quaternary Sediments of Western Turkmenistan of paleosecular variations in the geomagnetic field in Pliocene–Quaternary sediments. The detrital nature

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