AMPLITUDE DEPENDENCE OF RESONANCE FREQUENCY AND ITS CONSEQUENCES FOR SCANNING PROBE MICROSCOPY


Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6

The headwaters of fluvial systems on the East SUPREME MULTIVIT WITH IRON European Plain between the boundaries of the Marine Isotope Stage 2 (MIS 2) and MIS 6 glaciations evolved during the last 150,000 years.At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holoce

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