depleted mantle
基本解釋
- 貧化地幔;虧損地幔
英漢例句
- Sr isotopes of the rhyolites suggest that the volcanic rocks were chiefly derived from the depleted mantle source. Such a characteristic of rhyolites is very rarely seen.
該區(qū)流紋巖其源區(qū)物質(zhì)主要來自于虧損地?;蚴怯尚鋷r漿演化經(jīng)分離結(jié)晶作用形成的流紋巖這一特征是十分罕見的。 - Integrated study indicates that the two protolith suites of mantle peridotites represent remnants after polyphase melting of differently depleted mantle in different tectonic environments.
綜合研究表明該兩套地幔巖原巖組合代表了不同虧損程度和不同構(gòu)造環(huán)境下多期熔融的地幔殘余。 - 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.
地球化學(xué)研究揭示,榴輝巖的原巖很可能是形成在大陸內(nèi)部構(gòu)造環(huán)境的拉斑玄武巖,而石榴石橄欖巖可能是起源于虧損的殘余地幔。
雙語例句
詞組短語
- depleted MORB mantle 虧損
- depleted d mantle 貧化地幔
- depleted mantle source 虧損的地幔源
- Nd depleted mantle model age Nd 虧損地幔模式年齡
- model age to depleted mantle 虧損地幔模式年齡
短語
專業(yè)釋義
- 虧損地幔
We chose Ln(Co*Cr*Ni), Nb/Ta, plumbum isotopes composition, neodymium isotope two stage model age of depleted mantle (T2DM) andεNd(t) indexs to express the information and give the introduction of theory in the relevant chapters.2.
筆者嘗試提出用Ln(Co*Ni*Cr)、Nb/Ta、鉛同位素、釹同位素二階段虧損地幔模式年齡(T2DM)及εNd(t)等地球化學(xué)指標(biāo)表達(dá)以上信息,并在相應(yīng)的章節(jié)對指標(biāo)進(jìn)行了理論介紹。 - 貧化地幔
- 虧損地幔端元