Both Wangangheng and Shigezhuang complexes strongly correlate with regional mineralization and diagenesis of complexes in northern part of Taihang mountains. It is obvious that the mineralization and diagenesis are controlled by circular structures and tectonic zones which strike in NNE, NE, SN, EWand NWdirection respectly, especially those tectonic zones in SNand NWdirection have strongest relationship with mineralization in the study area. The structure dominate the emplacement and distribution of intrusions and, partial boundary and geometrical pattern of complexes. The Structure can become the host structure and control the distribution of altered rocks.