摘要
Through a sampling analysis of trace elements and REE in the section of Middle Permian Zhesi Formation in Solon area of Inner Mongolia,it is found that the overall sandstone and mudstone samples are characterized by LREE-enrichment. By analysis of the discriminant index of the sedimentary environment,the tectonic setting of Zhesi Formation is determined to be a continental island arc environment. Meanwhile,according to the sedimentary structure and lithology combination,Zhesi Formation is divided into the neritic-bathyal retention-reduction environment as well as the delta front and prodelta sedimentary systems.
Through a sampling analysis of trace elements and REE in the section of Middle Permian Zhesi For- mation in Solon area of Inner Mongolia, it is found that the overall sandstone and mudstone samples are charac- terized by LREE-enrichment. By analysis of the discriminant index of the sedimentary environment, the tectonic setting of Zhesi Formation is determined to be a continental island arc environment. Meanwhile, according to the sedimentary structure and lithology combination, Zhesi Formation is divided into the neritic-bathyal reten- tion-reduction environment as well as the delta front and prodelta sedimentary systems.
