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Experience of applying geochemical methods for determining palaeosalinity and palaeotemperatures to the study of Quaternary deposits of the Kola Peninsula
Abstract. The paper shows that geochemical indicators generally do not allow determining the salinity of the basins water that accumulated interglacial and interstadial sediments of the Kola region. The exception is boron subject to delineation of sediments with di- and trioctahedral illite. The time variation of summer water temperatures of an interglacial reservoir determined by geochemical methods agrees with palaeontological data.
Keywords: geochemistry, palaeosalinity and palaeotemperatures of waters, Quaternary deposits, the Kola region
Printed reference: V.Ya. Yevzerov Experience of applying geochemical methods for determining palaeosalinity and palaeotemperatures to the study of Quaternary deposits of the Kola Peninsula // Vestnik of MSTU. 2014. V. 17, No 2. P. 279-285.
Electronic reference: V.Ya. Yevzerov Experience of applying geochemical methods for determining palaeosalinity and palaeotemperatures to the study of Quaternary deposits of the Kola Peninsula // Vestnik of MSTU. 2014. V. 17, No 2. P. 279-285. URL: http://vestnik.mstu.edu.ru/v17_2_n57/279_285_yevze.pdf.
