Three-component Mixing Model of Isotopes and Trace Elements in Mantle Reservoirs

被引：5

作者：

李献华 ^{[1
]}

刘北玲 ^{[1
]}

机构：

[1] Institute of Geochemistry Academia Sinica

来源：

ChineseJournalofGeochemistry(EnglishLanguageEdition) | 1986年 / 02期

关键词：

Pb; Nd;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

Since 1970’s isotope and trace element studies of Cenozoic basalts provide evidenceof a heterogeneous mantle with a two-layer structure.J.B.Schilling and S.S.Sun etal.first proposed a two-layer model for the mantle and accounted with the conceptof“plume”for the mixing between the lower mantle and the depleted upper mantle,aswell as the differences in isotopes and trace elements among basalts.Especially since R.K.O’nions pointed out the negative correlation between Nd/Sr isotopes in oceanic basalts,many authors have justified such a correlation by using a two-component mixing model

引用

页码：123 / 139

页数：17