Monazite U-Th-Pb dating plays an important role in isotopic geochronology study. Identification of the genesis and interpretation of the age for monazites are the points. The internal texture, mineral assemblage, REE and trace element features are compared in detail in the paper to determine the identification of magmatic, hydrothermal and sedimentary monazites. In addition, they are both distinguished from magmatic monazites by their low trace elements content, Th/U ratio which has no stable correlation with that in zircon, enrichment in ∑REE and La, Ce, relatively poor in light rare earth elements and Sm, and Gd, and display typical tetrad effect REE distribution pattern.