文摘
Seismostratigraphic analysis of Paleogene deposits in northeastern Ustyurt was carried out. Four seismostratigraphic complexes have been recognized: Paleocene¨CYpresian, Lutetian¨CBartonian (Tasaran unit), Bartonian¨CPriabonian (Saksaul¡¯skaya¨CChegan), and Oligocene. We have established for the first time the clinoform structure of the Tasaran and Saksaul¡¯skaya¨CChegan complexes, which explains various concepts of their age. Seismostratigraphic analysis must be an integral part of stratigraphic research, which will significantly increase the reliability of correlation between geological sequences.