摘要
米仓山地区结晶基底的变质岩系中深熔作用发育，浅色条带与韧性剪切变形变质带关系表明，深熔作用和混合岩化作用受韧性剪切变形变质作用控制，而非超深变质作用的产物。
Relations between leucosome layers and ductile shear deformation metamorphic zones show that anatexis and migmatization was controlled by delctile shear deformation metamorphism,it did not occurred synchronously with ultrametamorphism
出处
《矿物岩石》
CAS
CSCD
北大核心
1998年第S1期111-115,共5页
Mineralogy and Petrology
基金
国家计委"八.五"重点攻关项目
