摘要
总结了近年来Ｏｓ同位素在示踪大洋玄武岩成因机制及大陆古老克拉通岩石圈地幔演化所取得的新成果和存在的主要分歧和不足之处，并对未来Ｏｓ同位素研究方向进行了展望。
The new achievements,main disagreements and insufficiency on Os isotope study in recent years are summarized in this paper.These achievements concenstrate in the origin of oceanic basalts and the evolution and petrogenesis of subcontinental lithospheric mantle xenoliths.The authors also look forward to the future in applied study on Os isotope.
出处
《地质科技情报》
CAS
CSCD
北大核心
1997年第3期93-96,共4页
Geological Science and Technology Information
