摘要
Xiangbai Formation was scarce of the fossil records, most parts were constituted of phytolite in South Guizhou Province. According to the lithologic,mineral and deposit characteristics of the neighborhood in the horizon of marine fauna, on the basis of the fossils’ identify with the palaeoecology method, the results showed that the marine fauna lived in a desalted lagoon which mainly located between Pingtang County and Dushan County. The barriers of lagoon and open sea were mainly located in the northeast of Baizhe-Mawei with NW extension. In the north part, Xiangbai Formation had evolved with the main flood plain deposits near the Tuchang. The structure within the lagoon was complete, and the limited low-energy environment could form well hydrocarbon source rock. Therefore, the distribution has great significance on the study of lithofacies and paleogeography as well as the assemblage of the source-reservoir-seal association in oil and gas fields.