摘要
大洋玄武岩中,元素之间常常存在线性关系.本文应用批式熔融模型,解释了这一现象.
On the basis of batch-type melting model, the author explains the linear relationships between elements which are often recognized in oceanic basalts.
出处
《地球科学》
EI
CAS
1987年第2期171-177,共7页
Earth Science
关键词
大洋玄武岩
批式熔融模型
线性关系
oceanic basalts
batch-type melting model
linear relationship
