Baitu AuPb Deposit is located at the intersection of the Kangshan - Shanggong Fault and Machaoying Fault on the southern margin of the North China Craton. The Au, Ag, and Pb ore bodies are in heterogeneous coexistence. They mainly occur in secondary fault zones in carbonate rocks in a vein-like and layered manner. This paper conducted rare earth and microelement tests on the main rocks. The characteristics of rare earth elements indicate widespread development of hydrothermal and metamorphic metasomatism. The specific characteristics are: w(REE) > 10 (REE) > 10(REE) >t(REEtek) > 10(REE mineralized dolomite) > 10W(REF-mineralind quarte vein), showing a feature of the greater the degree of alteration mineralization, the lower the total rare earth content; 2 The rare earth distribution curve shows that with mineralization, slope increases, enrichment degree of light rare earth decreases, and enrichment degree of heavy rare earth increases; 3 The influence of alteration on Eu element anomalies in rocks such as andesite tectonic rock and marble is not significant, while mineralization results in a significant negative anomaly of Eu element. Additionally, the alteration has a significant impact on Ce element anomalies in andesite, tectonic rock, and marble, causing the Ce element to evolve gradually from positive anomalies to negative anomalies. Mineralization further increases the degree of negative anomalies in Ce elements. Comparing the microelements of the main rocks and ores with that of the North China continental crust, it was found that andesite and marble are the main host rocks, and the ore-forming elements Ag. Sh, Pb, W, and Zn are enriched, providing high background value for lead mineralization. After alteration, Pb and W elements in andesite show obvious enrichment, suggesting that the hydrothermal fluid itself carries Ph and Wore-forming elements or has a hydrothermal metasomatic enrichment effect on the ore-forming elements in the wall rocks; In terms of anomalous intensity, tectonic rocks, quartz veins, quartz syenites, and (marble) dolomite have higher enrichment or depletion intensity compared to andesite rocks, and the anomalous intensity is sequentially strengthened, indicating a close relationship between the source of ore-forming matters and the carbonate rocks of Longjiayuan Formation. In summary, the genesis of Baitu AuPb Deposit is generally dominated by magmatic hydrothermal filling and metasomatism, but it is superimposed with later continental volcanic sedimentary transformation [ABSTRACT FROM AUTHOR]