SIVIRIS FORMATION (UPPER OLIGOCENE - LOWER MIOCENE), A NEW LITHOSTRATIGRAPHIC UNIT, KASSANDRAS PENINSULA (CHALKIDIKI, NORTHERN GREECE)

Kristalina Stoykova (1) , Ivan Zagorchev (1) , Jean-Pierre Suc (2)

1 Geological Institute of BAS
2 iSTeP - Institut des Sciences de la Terre de Paris

Upper Oligocene - Lower Miocene marine sediments are found and proven for the first time in Chalkidiki Peninsula. They are designated as Siviris For- mation and are dated by their calcareous nannofossil content.

Domaines: Sciences de la Terre

Kristalina Stoykova, Ivan Zagorchev, Jean-Pierre Suc. SIVIRIS FORMATION (UPPER OLIGOCENE - LOWER MIOCENE), A NEW LITHOSTRATIGRAPHIC UNIT, KASSANDRAS PENINSULA (CHALKIDIKI, NORTHERN GREECE). Comptes rendus de l'Académie bulgare des Sciences, 2012, 65 (8), pp.1117-1124. ⟨hal-00796926⟩