EM:富集地幔
“富集地幔”(Enriched Mantle)在学术及专业场景中常简称为“EM”,以便于快速书写和引用。该术语广泛用于地球科学、地质学等多个综合研究领域,用以描述一种具有特定地球化学特征的地幔物质类型。目前尚未形成严格的分类体系,但已成为相关文献中的常见表达。
Enriched Mantle的英文发音
例句
- REE and trace elements indicate that fluid came from enriched mantle.
- 稀土和微素元素地球化学研究显示流体源自富集地幔(EM);
- Some differences are found in O and C isotopic composition between phenocryst apatite and typical mantle materials, but the apatite is similar to that from the enriched mantle.
- 而碳酸岩的碳氧及斑晶磷灰石的锶、钛同位素组成与典型地幔物质有差异,与富集地幔(EM)颇为近似,从而证实在山东地区陆壳下存在富集地幔(EM)源区。
- Sr, nd and Pb isotopic characteristics of Early Cretaceous basaltic rocks from the coast of Zhejiang and fujian : evidences for ancient enriched mantle source
- 浙闽沿海早白垩世玄武岩锶、钕、铅同位素特征&古老富集型地幔的证据
- This ophiolite has higher REE and trace element abundances, suggesting it was derived from the enriched mantle.
- 该蛇绿岩有高的稀土和微量元素丰度,表明其来源于富集地幔(EM)。
- Element geochemical modelling indicates that both alkaline OIB and E-MORB samples were generated from the enriched mantle source.
- 元素的地球化学模拟表明,碱性OIB和E-MORB样品是来自较原始地幔还要富集的地幔源区。
本站英语缩略词为个人收集整理,可供非商业用途的复制、使用及分享,但严禁任何形式的采集或批量盗用
若EM词条信息存在错误、不当之处或涉及侵权,请及时联系我们处理:675289112@qq.com。