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磐石圈岭透闪石矿床特征及开发前景
引用本文:张国强,于政涛,刘东伟,刘振宇.磐石圈岭透闪石矿床特征及开发前景[J].吉林地质,2005,24(2):35-39.
作者姓名:张国强  于政涛  刘东伟  刘振宇
作者单位:1. 吉林省磐石市地质矿产管理局,吉林,磐石,132300
2. 吉林省地质调查院,吉林,长春,130061
摘    要:圈岭透闪石矿床位于磐石——双阳褶争束东南段,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。

关 键 词:透辉透闪石矿  矿床特征  磐石圈岭
文章编号:1001-2427(2005)02-035-05
收稿时间:2004-11-05
修稿时间:2004-11-05

The deposit characteristics of the Quanling tremolite, Panshi area, and its developing prospect
ZHANG Guo-qiang,YU Zheng-tao,LIU Dong-wei,LIU Zhen-yu.The deposit characteristics of the Quanling tremolite, Panshi area, and its developing prospect[J].Jilin Geology,2005,24(2):35-39.
Authors:ZHANG Guo-qiang  YU Zheng-tao  LIU Dong-wei  LIU Zhen-yu
Abstract: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.
Keywords:pitkarandite  deposit characteristics  Quanling of Panshi area
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