Abstract
Abstract Describes the stratigraphic sequences and structure of the Pelagonian and Vardar zones in Greek Macedonia. The eastern and western borders of the Vardar zone had a substantially different history of development in the Mesozoic; only after the beginning of the Priabonian (Eocene) did both depositional areas subside together, to be covered by Molasse deposits. It is thus only from Priabonian time that the Vardar zone in Kossmat's sense became differentiated; it is essentially a hinterland trough whose individualization took place after the major Hellenide tectonic movements.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
