摘要
Caixiashan deposit, which belongs to sedimentary alteration type, is the only large Pb-Zn deposit in middle Tianshan area at present. Clastics and carbonate formation which is in the first member of Kawabulake group, magmatic hydrothermal of Variscan and subfaults of Aqikekuduk fault control the forming of the deposit. The positioning of ore bodies is correlated with geo-anomaly. Mineral prediction could be conducted by the delineation of geo-anomaly units. Through the quantative study of geo-anomaly, large scale metallogenic prognosis was completed in Caixiashan deposit, which proved that there were great potential for mineral exploration in the area.