The Shanghuangqi-Wulonggou faulted belt is an important tectonic-magmatic-metallogenic belt in North China. Based on 1:250000 stream sediment geochemical survey in Weixian Sheet of Hebei Province, the authors obtained content data of 39 kinds of elements for factor analysis, and made an analysis of stream sediment geochemical anomalies in Zoumayi-Dahenan area along Shanghuangqi-Wulonggou faulted belt. The three geochemical anomaly series of Mo-W-Bi-Cu, Pb-Zn-Ag-Cd and Au-Hg-Agshow very intimate relationship with regional structure, magmatic rocks and metallogenic process. The results obtained by the authors effectively solve the problem of the difficulty in determining element association and spatial distribution of the anomaly due to the superimposition of various elements and hence can provide reference for arrangement of geochemcial exploration and study of regional metallogenic regularity.
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