The assemblage of garnet-diopside in the silicate alteration rocks is different from that in the skarn of traditional id硅酸盐蚀变岩中的“石榴子石－透辉石”组合与传统理解的“夕卡岩”内的相同组合名同实异。
The auriferous skarn deposits and copper (associated with gold) skarn deposits discovered in the past ten years are also近十年来，我国所发现的含金夕卡岩矿床和铜伴生金夕卡岩矿床也主要产在长江中下游地区。