抄録
Jurassic and Cretaceous granitoid bodies are widely distributed in the Sanandaj-Sirjan Zone (SaSZ) of the Zagros Orogen. The Shalair Valley granitoid plutons in NE Iraq are located within Iraqi Zagros Suture Zone which is considered as an integral part of SaSZ in Iran, and several types of granitoid are distributed there. In this study, we reported radiometric ages and chemical and Sr-Nd isotopic features of the Shalair Valley granitoids.