The Quruqtagh area, a place which the Tushibulake Formation was named and in which typical geological sections are distributed,  contains a clastic sedimentary succession consisting mainly of grayish sandstones, siltstones, tuffaceous sandstones and siltstones, and minor limestones. U-Pb ages of detrital zircons from three sandstone samples were measured using the LA-MC-ICP-MS method. The study of detrital zircons shows that regional metamorphism developed within this area may result partially from the supercontinent Columbia.