摘要
敦化鸡血玉矿位于富尔河—古洞河大断裂西南段,产于海西期黑云母斜长花岗岩中,属低温热液裂隙充填型矿床,矿石类型以角砾状、块状及条带状为主,主要用于观赏石、图章石、首饰及各种摆件。
The Dunhua bloodstone deposit is located in the southwestern part of the Fuerhe- Gudonghe fault, which occurred in the Hereynian biotite plagiogranite, and which belongs to epithermal fracture filling ore deposit; the ore types show mainly breeeiform, massive and banded structures, it was mainly used in decorative stone, stamp, woman＇s personal ornaments and ornaments for furnishing and decorating.
出处
《吉林地质》
2005年第4期54-58,共5页
Jilin Geology
关键词
鸡血玉
矿床特征
敦化
bloodstone
features of ore deposit
Dunhua
