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Development of sediments in this part of the KleszczГіw Graben in the Pleistocene was largely influenced by tectonic factors (Chabielice fault, DД™bina Salt Dome) and glacitectonic processes (Wartanian Glaciation). The studies were carried out in 2014вЂ“2016 and resulted in both establishing the sedimentary Saalian complex and constructing geological cross-sections and a synthetic lithostratigraphic profile. Laboratory studies included macrofossil analysis of the deposits, as well as petrographic and geochemical (neodymium isotope ratio) measurements. The study area is located in the SzczercГіw outcrop, BeЕ‚chatГіw Lignite Opencast Mine, central Poland. This paper presents the results of new studies of Saalian tills, from the ЕЃawki and Rogowiec formations, filling the KleszczГіw Graben.

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Introduction to genetic principles pdf viewer