Saneh-Shahabad Ophiolite has an intra-plate oceanic arc to island arc chemical signature as for Desmons and Beccaluva in 1983 and has to have a Llte cretaceous age as 5: 2., 7. and eight., Ali et al. (2014) associates to this ophiolitic top with mafic unit Γ tectonically during the Avroman Formation in Avroman Mountains.
The Saneh-Shahabad Ophiolite has an intra-plate oceanic island arc to island arc chemical signature (e.g. Desmons and Beccaluva, 1983) and has been assigned a Late Cretaceous age (Figures 2, 7 and 8). Ali et al. (2014) associated this ophiolitic body with a mafic unit, tectonically overlying the Avroman Formation in the Avroman Mountains.