摘要
岩浆岩的含钾性主要取决于岩浆起源地区的区域变质程度。它是控制金属成矿分区的重要因素之一。
The K-bearing property of magmatite are mainly dependant on the degree of regional metamorphism in the juve-nile area(where magma originated),which controls the metal metallogenic province and is one of the important fac-tors.
出处
《地质与勘探》
CAS
CSCD
北大核心
1994年第1期1-6,共6页
Geology and Exploration
