Morave Mt Oligocene-Middle Miocene succession of Albanian-Thessalian Basin | Zendy

Pandeli Pashko | Zendy

AI Assistant Blog Pricing

Home ZAIA Blog

Open Access

Morave Mt Oligocene-Middle Miocene succession of Albanian-Thessalian Basin

Author(s) -

Pandeli Pashko

Publication year - 2018

Publication title -

bulletin of the geological society of greece

Language(s) - English

Resource type - Journals

eISSN - 2529-1718

pISSN - 0438-9557

DOI - 10.12681/bgsg.15837

Subject(s) - molasse , geology , paleontology , structural basin , ecological succession , unconformity , middle miocene disruption , foreland basin , fauna , late miocene , ecology , biology

The Morava Mountain Oligocene-Middle Miocene molasse deposits take part in the Albanian-Thessalian Basin, which developed NW-SE from eastern Albania to Thessaly in Greece, where it is called as Mesohellenic Basin. The 4.5 km thick basin infill is subdivided into three molasse cycles separated by two regional unconformities at the Eocene/Oligocene and Aquitanian/Burdigalian boundaries. The Morava Mountain Oligocene-Middle Miocene molase, ~ 3500 m thick, represents an exposed continuous, rich in fossil fauna succession. Six stratigraphic sections were studied and measured.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.

Having issues? You can contact us here

Accelerating Research