Weikuang gold deposit in Qixia city occurs in monzonitic granites of Guojialing superunit in early Yanshan period. Its mineralization is controlled by the structure with the trend of NE strictly, and mainly composed of berestie mylonite and beresite fragmented rocks. Orebodies occur in vein and phacoidal type. Through analysis of controlling conditon on structure, rock and alteration, it is regarded that this area has gold-forming future.