黑龙江伊春西南锅盔山一带属于黑龙江省重要的铁多金属(金银)成矿带,是兴蒙造山带东端中生代“花岗岩海”的一部分。近年在该地区发现了与早中生代花岗岩有关多金属矿床、矿(化)点近十处,矿床成因类型有斑岩型、夕卡岩型、岩浆期后热液型等(图1),因而具有形成超大型多金属矿田的潜力而受关注(韩振新等,2004;葛文春等,2007;时永明等,2007;韩振哲等,2009;2010)。 Heilongjiang Yichun southwest of the mountain area is a key area in Heilongjiang Province iron polymetallic (gold and silver) metallogenic belt, is the eastern end of the Xingmeng orogenic belt “granite sea ” part. In recent years, many polymetallic deposits related to the Early Mesozoic granites have been discovered in this area. Nearly ten ore mined (ore-forming) sites have been formed, and their genetic types include porphyry type, skarn type and post-magmatic hydrothermal type (Figure 1) With the potential to form very large polymetallic ore fields (Han et al. 2004; Ge Wenchun et al. 2007; Shi Yongming et al. 2007; Han Zhe Zhe et al. 2009; 2010).