RESULTS OF MAGNETOSTRATIGRAPHIC STUDY OF THE LOWER SYZRAN SUBFORMATION (PALEOCENE) IN THE NORTH OF THE SARATOV RIGHT BANK (GREMYACHKA AND KLUCHY-2 SECTIONS)

Results of magnetostratigraphic study of the Lower Syzran subformation (Paleocene) in the north of the Saratov Right Bank (Gremyachka and Kluchy-2 sections)

Results of magnetostratigraphic study of the Lower Syzran subformation (Paleocene) in the north of the Saratov Right Bank (Gremyachka and Kluchy-2 sections)

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The results of petromagnetic and paleomagnetic studies of two sections of the Lower Syzran subformation (Paleocene) – Gremyachka and Klyuchi-2, located in the north Satellite Coffee Servers of the Saratov Right Bank and represented by weakly magnetic silicites, are presented.Paleomagnetic data on sections, despite their low quality and fragmentation, are important for magnetostratigraphy, because they Equipment Stands confirm the presence of a reverse polarity magnetozone (analogous to chron C27r and/or C26r) in the Lower Syzran subformation and its lateral stability.

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