Significance of phosphorous (P)- and magnesium (Mg)-bearing high-Al titanite in high-pressure marble from Yangguantun,Rongcheng County, Shandong Province

被引：2

作者：

叶凯

叶大年

机构：

来源：

ChineseScienceBulletin | 1996年 / 14期

基金：

中国国家自然科学基金;

关键词：

high-Al titanite; P- and Mg-bearing titanite; high-pressure marble; Shandong;

D O I：

暂无

中图分类号：

P578 [矿物分类];

学科分类号：

070901 ;

摘要：

Titanite is a widespread accessory mineral in metamorphic rocks. The united exchange Ti+O=(Al, Fe)+(OH, F) is now recognized as a common substitution in metamorphic titanite. Five theoretical titanite end-members were recognized by Smith: CaTiSiOO (oxy-titano-titanite), CaAlSiOOH (hydroxy-alumino-titanite), CaAlSiOF (flour-aluminotitanite), CaFeSiOOH (hydroxy-ferri-titanite) and CaFeSiOF (flour-ferri-titanite). The

引用

页码：1194 / 1197

页数：4