Paleomagnetic studies of upper Neopleistocene rocks from the El’tigen cross section, Kerch Peninsula
Journal: Geomagnetism and Aeronomy
Year: 2015

The upper part of the Neopleistocene El’tigen cross section was studied by the paleomagnetic method. The cross section is located in the Crimean Peninsula, on the shore of the Kerch Strait, and is composed of Surozhian deposits referring to the time interval of ~15–45 kyr B.P. Detailed ChRM angular element curves were obtained, and virtual geomagnetic pole migration curves were constructed. On the basis of these data, singular anomalous intervals (~23–25, ~33–35, and ~41–42 kyr B.P.) were distin