Data from: Petrogenetic studies of Permian pegmatites in the Chinese Altay: implications for a two-stage post-collisional magmatism model

Understanding the petrogenesis of rare-metal pegmatites is important for
understanding ore-forming processes and their tectonic settings. In this
study, we performed zircon U-Pb geochronological and Hf-O isotopic
analyses of the Xiaokalasu (XKLS), Dakalasu (DKLS) and Yelaman (YLM)
pegmatites in the Chinese Altay orogen. These pegmatites have low εHf(t)
values (-0.6 ~ +4.3), two-stage model ages of 989 ~ 1293
Ma, and high δ18O values (+6.52 ~ +11.31), indicating that they
may have been derived from the anatexis of mature sedimentary rocks in the
deep crust, with a small amount of mantle-derived or juvenile material.
Geochronological and Hf-O isotopic data for granitic intrusions
in the Chinese Altay Mountains indicate that the εHf(t) values
decreased from the Permian to the Triassic, which implies
that two-stage post-collisional magmatism occurred in this
region. During the Permian, the thin lower crust was cold; thus, magmatism
likely originated in the deep crust close to the Moho surface and involved
intense mantle-crust interactions. During the Triassic, asthenospheric
upwelling provided heat to the lower crust, which increased the geothermal
gradient and led to the anatexis of shallow crustal material.