///This paper discussed effects of the Emei Mountains plume activity on sedimentary paleographical features and sedimentary-facies distribution during the Xixia period of Mid-Permian. The studying area is a sub-facies open-platform developing area, located at the higher part of the submarine dome-shaped area in the southwestern Upper Yangtze platform, and gradually transformed eastward and northeastward into the ramp-facies developing area. The paleogeographical pattern and sedimentary facies distribution during the Xixia period in this area can be regarded as the early developing stage from carbonate ramp to platform, which provides part evidence for the activity of the Emei Mountains mantle plume.