Writers : Gol Gir e Noosh Abadi, Z.; Vahidi Nia, M.; Ashoori. A. R.
Refference : 28th Symposium on Geosciences and the 14th Symposium on Geological Society of Iran
Publishing Year : 1389

Abstract :

Eocene sediments at the Tange-Olia in the Western – North of Neyshabur area contain alternations of marl, sandstone and conglomerate. In this study sediments have 398 meters (thick) that lower contact is disconformity with Jurrasic and upper contact reaches to Neogene red bed. Several genera and species of benthic and planktonic foraminifera are recognized that 7 species are Nummulites. This assemblage indicates lower to upper Eocene for these deposits.

Subject List : stratigraphy