marl and marly lime accompanied by layers of fossiliferous limestones. This formation lays
conformably over the Haft-Tuman Formation, while its upper boundary is disconformable
with Chupanan Formation. In this study, 23 rock samples from marl segment of the Farokhi
Formation were prepared palynologically and their various palynological constituents were
characterized and quantified by percent. Assessing the organic elements of formation …