摘要
Xiaorequanzi Formation is a unit of volcanic rock among Carboniferous-Permian volcano-sedimentary rocks which are widely exposed in Queletag, East Tianshan Mountains, Xinjiang. It has been divided into Early Carboniferous by referring the neigboring Digar Formation which is defined to Middle Carboniferous by fossil age. Different ages have been given on Xiaorequanzi copper mine in the southern part of Queletag. In the northern part, isotopic chronology data is absent where it is dated by using SHRIMP. According to present evidence, Xiaorequanzi Formation ought to be Early Permian and other strata units and their relative age may be renewed.