The Govanda Formation was deposited during the Early-Middle Miocene Epoch in intermountain areas between Zagros Suture and Imbricate zones. Paleoecology depositional environment of has been studied detail Mergasor Penjwen districts for first time. formation these two sections from bottom to top is comprised thick bedded, oyster chert bearing conglomerate, pebbly sandstone, red-brown shale silts...