Abstract
A number of properties of basal clays is shown to be retained by the weathering products that have developed on them in the Stavropol region. Tertiary eluvial and Quaternary deposits formed in the arid zone have thus inherited from the basal Maikop clays a high degree of dispersion, the composition of exchangeable cations and the mineral composition of the clay fraction.
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Schedule a callMore From: Bulletin of Engineering Geology and the Environment
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