Paleomagnetic studies of Quaternary sedimentary rocks in seaside outcrops near the Shirokino - Bezimenne villages (Donetsk region) and Kulikovskoe village (Zaporizhia region) from the Priazovian area have been carried out. The standard procedure of the samples demagnetization by alternating magnetic field and temperature, the isolation of the characteristic J0n component by the method of the Kirshvink analysis were used to acquire the initial data of further paleomagnetic structures. An analysis of the obtained results allows to define the Matuyama-Brunhes boundary at the level of deposits of Martanosha stratigraphic horizon, and we can find at least eight reversed polarity intervals in Brunhes Chron.

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