Taking the sediments of Shenzhen urban mangrove wetland as the research object, the mineral composition and physical and chemical properties of the sediments are analyzed, and the characteristics of mineral composition and influencing factors are explored. The main results show that the whole rock mineral composition in surface sediment is given priority to clay minerals (16.5%?73.5%) and quartz (22.0%?81.2%), and there are differences in the contents of potash feldspar, pyrite, and rock salt in different samples at different depths. The main types of clay minerals in surface sediments are imonite (44%?76%), kaolinite (0%?40%), chlorite (0%?24%), and illite (2%?21%), and are dominated by imonite. The distribution characteristics of clay minerals at different depths are basically the same as those in surface sediments. There are significant differences in the composition of clay minerals in the sediments of the Pearl River Estuary and Daya Bay without vegetation. Correlation analysis shows that the composition of whole rock minerals is mainly affected by salinity, TS and TOC, while the composition of clay minerals is mainly affected by pH, salinity, TOC, and sediment particle size.