///In order to understand the regularity of enrichment and dispersion of geochemical elements in rocks and other media, this paper uses multifractal and geostatistic methods to analyze their spatial association and singularity;the multifractal method can be carried out in multifractal modeling; and the geostatistics can be applied using variogram. The paper uses these two methods to analyze 1∶50 000 drainage sediment geochemical data; the case study introduced in the current paper indicates that the local singularity in this area can reflect the alteration or other favorable location for mineralization. In order to make a further study about the relationship between anomaly and singularity, spectrum-area method is used to analyze the main ore-forming elements Pb and Z. It indicated that the abnormal area obtained from S-A is in accordance with the singularity area, and that the abnormal has the characteristics of a local singularity. The study area with singularities is an enrichment area that contains lead zinc-copper anomaly; the singularities are related to the mineralization and the occurrence of known deposits, which provide important clues for mine potential evaluation.