magyarországi quarter es pliocén szárazföldi biosztratigráfiának vázlata (Sketch of the Late Cenozoic (Pliocene and Quaternary) terrestrial stratigraphy of Hungary). - Földr. Közl., 93/3, pp. 179-204. (in Hungarian) A magyarországi
Quaternary relief evolution of various volcanic areas in Hungary has been determined by (a) the original volcanic succession and related, primary landforms and (b) the subsequent postvolcanic tectonism and erosion. This overview presents some details of these processes through selected relief types from the Miocene volcanic mountains of Hungary: the High Börzsöny erosional caldera rim, the Rocks of Vadálló-kövek, the Dobogókõ Ridge, the Danube Bend area, and the badlands and fairy chimneys of the southern foreland of the Bükk Mts, by showing different volcanic relief types, and postvolcanic tectonic, paleogeographic and erosional history. In the Quaternary, the tectonic transformation of these and other volcanic areas has been highly variable; in contrast, erosional processes of the Quaternary, i.e. pedimentation, loess and other eolian sedimentation, derasion, periglacial relief formation, and channel erosion, have affected almost all areas in Hungary; hence types and rates of erosion can be well constrained.
Korpás, L., P. Kovács-Pálffy, M. Lantos, M. Földvári, L. Kordos, E. Krolopp, D. Stüben, Zs. Berner (in press): Sedimentology, geochemistry, chronology and palaeokarst evolution of a Quaternary thermal lacustrine travertine. An integrated case study from
133 Bell, M., J.C.W. Walker 1992: Late Quaternary Environmental Change. -- Longman Group, Hong Kong. Late Quaternary Environmental Change
approach is proposed to get GPC from natural soybean lecithin catalyzed by the quaternary ammonium base resin made in our laboratory. To analyze the process of the transesterification easily, excess methanol was used as reactant and solvent to form a
Quaternary thermal lacustrine travertine. An integrated case study from Vár-hegy, Budapest, Hungary. -Karsztfejl\H{o}dés, 7, Szombathely Paulik, J., F. Paulik, M. Arnold 1987: Derivatograph-C. A microcomputer
693 Buffet-Bataillon S, Tattevin P, Bonnaure-Mallet M, Jolivet-Gougeon A: Emergence of resistance to antibacterial agents: the role of quaternary ammonium compounds — a critical review. Int J
Quaternary pyridinium aldoximes have been analyzed by thin-layer chromatography. Their separation was adequate when silica plates were used with a mobile phase with a high water content. As a consequence of their limited migration, reversed-phase TLC was not appropriate for determination of the lipophilicity of quaternary pyridinium aldoximes. Displacement TLC of some quaternary pyridinium aldoximes is, nevertheless, possible using silica as stationary phase with water-acetone-hydrochloric acid mobile phases. Normal-phase TLC with different concentrations of organic modifier gave a series of R M values for the pyridinium aldoximes. Approximation of the different plots of R M against organic modifier concentration to straight lines afforded R M,0 values and the slopes of the lines. The R M,0 values and the slopes both serve as indicators of the hydrophilic character of the compounds.
Ökológus Kongresszus, Elodblac;adások és poszterek összefoglalói, Gödollodblac;, p. 126. Katz, N., J., S. V. Katz, M. G. Kipiani 1965: Atlas and keys of fruits and seeds occurring in Quaternary deposits of the USSR
Abstract
The extraction of Np(IV), Pu(IV) and U(VI) from aqueous hydrochloric acid into quaternary amines has been studied. The dependence of the distribution coefficient on amine concentration suggests that the actinide ions extracted are NpCl 6 2− PuCl 6 2− and UO2Cl 4 2− . This is further supported by the absorption spectra of the amine extracts of these actinide ions. Based on the extraction data obtained, a simple method for the separation of typical metal ions such as Cs, lanthanides and Zr from U(VI) and Pu(IV) is suggested.
