The OligoceneeMiocene Qom Formation has different depositional models in the Central Iran,SanandajeSirjan and Urumieh-Dokhtar magmatic arc provinces in Iran.The
The Khok Kruat Formation is the upper part of the Khorat Group, which consists of upper Lower Cretaceous non-marine sedimentary rocks in northeastern Thailand.
Magma mixing process is unusual in the petrogenesis of felsic rocks associated with alkaline complex worldwide.Here we present a rare example of magma mixing in
The Ching-dar syncline is located to the west of the city of Birjand,in the east of Iran.The ca.500 m thick studied section at the eastern flank of the syncline