Abstract
A high-resolution cyclostratigraphy and magnetostratigraphy is presented for the Messinian lacustrine Lava section
from the Servia Basin in NW Greece, constraining more precisely the absolute ages of magnetic polarity subchrons
C3An.1n and C3An.2n. The section contains 15 distinct sedimentary cycles of alternating dark- and light-coloured
marls, while the gamma-ray attenuation record reveals an
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