摘要
圈岭透闪石矿床位于磐石—双阳褶皱束东南段,产于中酸性岩浆岩与石嘴子组碳酸盐沉积建造的接触蚀变带内,属矽卡岩型矿床,矿石类型以透辉透闪石矿为主,主要应用于陶瓷工业。
The Quanling tremolite deposit is located in the southeastern part of the Panshi- Shuangyang fold cluster, which is occurred in the contact alteration zone of intermediate acidity magmatic rock and Shizuizi Formation carbonate sedimentary formation, and which belongs to skarn type deposit. From ore type, the tremolite is dominant, which mainly applies it to ceramic industry.
出处
《吉林地质》
2005年第2期35-39,共5页
Jilin Geology
关键词
透辉透闪石矿
矿床特征
磐石圈岭
pitkarandite
deposit characteristics
Quanling of Panshi area
