Geochronological databases are powerful tools for characterizing the crustal evolution and the age spectra of a region and allow comparison with other areas at a regional scale. In this contribution,
A compiled dataset of detrital zircon ages (ds01) and Hf isotope data (ds02) from the Tengchong, Lhasa, Sibumasu, and South-Qiangtang blocks, spanning 300 to 100 Ma. The data used in this study were d
