SHRIMP U-Pb dating of zircons from two representative samples of the batholith shows that the crystallization age is (473.5±2.9) Ma and (461.5±7.3) Ma, respectively. Petrochemical and geochemical analyses show that the magma of the granite was derived mainly from the melting of the upper crest. The authors come to the conclusion that the emplacement and crystallization of the granite batholith had a close relationship with the collisional orogeny and crustal thickening and were also closely related to the crustal partial melting in the late period of the Pan-African orogeny.