1) mantle end members
地幔端员
1.
It is thought that there are no common mantle end members of EM1,EM2 and HIMU, which only occur individually at very local areas, and their source region is probably related to a transition zone between the u.
笔者认为不存在具有公共性质的EM1、EM2和HIMU地幔端员,它们的源区可能来自上、下地幔过渡带,只在局部地区出现,独一无二。
2) mantle component
地幔端元
1.
This presentation reports the new improvements of Lu Hf isotope study on some of the mantle components.
报道了Ｌｕ－Ｈｆ同位素体系在地幔端元的地球化学研究中的部分最新应用成果。
3) EM2 mantle component
EM2地幔端元
4) mantle domains
地幔端元组分
1.
Based on research results at home and abroad, this paper studies the geochemical characteristics of trace elements of mantle domains such as DMM, HIMU, EM1 and EM2 defined by isotopic geochemistry, and discusses the genesis of those end-member components.
结合国内外研究现状，对利用同位素地球化学所确定的地幔端元组分DMM、HIMU、EM1和EM2在微量元素地球化学上的特征进行了综述，并对其成因进行了讨论。
5) EMI type mantle
EMI型地幔端元
6) mantle
[英]['mæntl] [美]['mæntḷ]
地幔
1.
A mineral assemblage of sulfides and sulfo-arsenides from the ophiolite mantle in Tibet;
来自蛇绿岩地幔的硫(砷)化物矿物组合
2.
Water content in the Earth s mantle .;
地幔中水的存在形式和含水量
3.
High Resolution Body-Wave 3-D Tomography of Mantle of China and Adjacent Areas;
中国及邻区地幔三维结构高分辨率体波层析成像
补充资料：地幔
| 地幔 earth mantle 地壳和地核之间的中间层。平均厚度为2800余千米 。1914 年 B. 古登堡根据地震波走时测定地核的深度为2900千米，比现代精密测量的结果只差15千米。因此，地核-地幔边界又称古登堡不连续面。 见地球内部构造。 |
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参考词条