“…The collision zone has exposed Mesozoic sediments, predominantly composed of limestone, with marble, alabaster and chert, as well as less commonly occurring gabbro, diorite and basalt (Karim et al 2009); nodules and cobbles of these materials have eroded from the rocky outcrops and can be gathered from the riverbeds (Jassim et al 1982;Al-Barzinjy 2008;Azizi et al 2013). The clay-rich deposits of the Mesopotamian plains and Zagros intermontane valleys are the result of orogenic activity, and the accompanying transgression and regression of the Tethys Sea (Khormali and Abtahi 2005;Abbaslou and Abtahi 2008;Godleman et al 2016). Clays are the common denominator in the settlements of the Neolithic, used for constructing dwellings, lining pits and baskets, and for making tokens, figurines and, in the late Neolithic, vessels and trays.…”