MAGNETIC-PROPERTIES AND PALEOMAGNETISM OF SEDIMENTS IN THE WESTERN SECTOR OF THE BLACK-SEA IN CONNECTION WITH SEDIMENTATION CONDITIONS IN LATE PLEISTOCENE AND HOLOCENE

Paleomagnetic episode Getenburg was registered in the new-evksinik sed iments right under the marking hydrotroilitic level and excursus etrus sion in jemitine sediments. By means of magnetic mineralogy it is show n that approximately to the middle of hydrotroilitic level the magneti c properties are controlled by magnetite, hematite and maggemite and h igher by the ferrosulphides. The two main peaks of sediments magnetizi ng were found in the upper part of the hydrotroilitic level and in the bottom of calamatic sediments. The observed variations correlate with the paleogeography of the region.