摘要
Based on the fundamental principle of strontium isotope stratigraphy, the authors analyzed the rock fabric and chemical composition, made preservative evaluation for coeval seawater of the carbonate rock samples near the Permian-Triassic boundary in the Huaying Mountain, eastern Sichuan Province, and then measured strontium isotopic composition of the samples. These samples haven’t suffered much from the strong diagenetic alteration and can represent preferably the coeval seawater,as evidenced by their relatively good original sedimentary fabric and high Sr concentrations. The application of strontium isotope stratigraphy to the Permian/Triassic boundary in the Huaying Mountain will provide some useful basic data for the chemo-stratigraphic and global correlative studies of marine Permian-Triassic boundary in South China.