Data for: Ultrahigh temperature metamorphism in the Dabie orogen during Triassic continental collision
Zircon U-Pb ages and trace elements in different domains such as Triassic metamorphic and Early Cretaceous anatectic domains are listed in the Tables 1 and 2. These data are focus on recongnizing the multiple metamorphism and metamorphic ages and temperatures during the orogenic evolution. The electron microprobe data of the mineral inclusions in metamorphic zircon domains are listed in the Table 3, in order to limit the metamorphic conditions such as accurate pressure. All these data suggest a Triassic granulite-facies UHT metemorphism during the continental collision.