摘要
Stratigraphic framework,tectonic framework and magmatic evolutionary series have been established in 1∶50 000 regional geological survey in Chengbu,southwestern Hunan Province. The deposition of Huangshidong Formation of Qingbaikouan system is at (828±10) Ma which is yielded by zircon SHRIMP U-Pb dating. According to the contact relationship, rock characteristics and the isotope ages new-acquired, the authors subdivided the granite-bodies in Chengbu area into 12 intrusive periods, 31 intrusive masses, and merged into four magmatic evolutionary series. The new discovery of gneissose granite of Qingbaikou period greatly improved the study of magmatic rocks in this area.