地质与资源2017，Vol.26Issue(2)：124-128,5.
内蒙古维拉斯托锡多金属矿床含矿斑岩体钾长石斑晶的有序度及成因探讨
THE ORDER DEGREE AND ORIGIN OF K-FELDSPAR PHENOCRYSTS IN THE MINERALIZED PORPHYRY OF THE WEILASITUO POLYMETALLIC DEPOSIT IN INNER MONGOLIA
摘要
Abstract
The study of order degree and structural temperature of K-feldspar can provide significant information about the forming physicochemical conditions of deposit.Infrared spectroscopy is used to test the K-feldspar phenocrysts from the mineralized porphyry in the Weilasituo polymetallic deposit.The result shows that the order degrees range from 0.85to 0.95,with triclinities of 0.7-0.9.The structural temperatures are 547.17-578.36 ℃,suggesting that the K-feldspar phenocrysts are microcline.It is confirmed that the K-feldspar is a product of hydrothermal alteration.关键词
钾长石斑晶/有序度/成因/含矿斑岩体/维拉斯托锡多金属矿/内蒙古Key words
K-feldspar/order degree/origin/mineralized porphyry/Weilasituo polymetallic deposit/Inner Mongolia分类
天文与地球科学引用本文复制引用
杨帆,汪岩,樊志勇,付俊彧,那幅超,张广宇,刘航..内蒙古维拉斯托锡多金属矿床含矿斑岩体钾长石斑晶的有序度及成因探讨[J].地质与资源,2017,26(2):124-128,5.基金项目
中国地质调查局项目“大兴安岭成矿带突泉-翁牛特地区基础地质综合研究与片区总结”(编号 DD20160048-1) （编号 DD20160048-1）
“古亚洲构造域东段构造格局、演化历史研究和1:250万构造图编制(编号 DD20160343-08). （编号 DD20160343-08）
