Located in the southern margin of South Qinling belt, the Dalangshan Group is a series of volcanic-sedimentary rocks and exposed well in Xinyangdain area of Suizhou City, Hubei Province. To find out the diagenetic age of the Dalangshan Group and provide credible time information on the materials in “Qinling microplate”, the authors carried out a detailed fieldwork on Dalangshan Group and collected representative schist samples to study petrography and LA-ICP-MS zircon U-Pb geochronology. The scattering of LA-ICP-MS zircon U-Pb ages suggest that the zircons from the schist of Dalangshan Group are detrital zircons and have not been obviously influenced by later greenschist-facies metamorphism.