DM:贫化地幔
为便于书写和使用,“Depleted Mantle”在地质学等学术科学领域常被缩写为DM。该术语的中文译名为“贫化地幔”,主要用于描述地壳形成过程中因部分熔融导致部分元素流失后所形成的地幔物质,是研究地球化学演化和岩石成因的重要概念之一。
Depleted Mantle的英文发音
例句
- The chemical characteristics indicate that the protolith of eclogites were possibly tholeiite with a continental affinity, whereas the garnet peridotites were derived from a depleted mantle.
- 地球化学研究揭示,榴辉岩的原岩很可能是形成在大陆内部构造环境的拉斑玄武岩,而石榴石橄榄岩可能是起源于亏损的残余地幔。
- The MORB and OIB of the Sanjiang area were generated from the depleted mantle and the primitive mantle respectively.
- 它们均属南半球地幔域。亏损地幔和近原始地幔分别是三江地区MORB和OIB的源区物质。
- Accordingly, the northern and southern parts of Xinjiang can be divided into two obviously different isotopic geochemical provinces : the northern province is characterized by isotopic compositions of the depleted mantle, whereas the southern province by isotopic compositions of the enriched mantle.
- 据此,可以将新疆南部和北部划分为两个明显不同的同位素地球化学省。南部省以富集型地幔的同位素组成为特征,而北部省以亏损型地幔的同位素组成为特征。
- The second source is the depleted mantle, which lies underneath the mid-eastern transform domain. Basalts from this source have low 87Sr / 86Sr isotopic compositions, lower REEs and trace elements and higher contents.
- 另一个是位于转换断层中-东部下面的亏损地幔,来自这个地幔源的玄武岩具有低87Sr/86Sr、低稀土元素和微量元素含量,但MgO含量较高。
- Trace element geochemistry and mineral chemistry studies on the metamorphosed harzburgite indicate that it is the relict of the depleted mantle.
- 变质方辉橄榄岩的微量元素地球化学及矿物化学特征表明,应为亏损的残余地幔产物。
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