REE in fluid ? melt inclusions of mantle xenolith from Changbaishan are measured directly by ICP? MS.
本文嘗試運用電感耦合等離子體質(zhì)譜(ICPMS) 和熱爆方法,直接測定了長白山地區(qū)的地幔捕虜體中流體熔體包裹體 REE 含量.
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As a new method, REE tracer technique has been widely used in soil erosion research.
REE示蹤技術(shù)作為一種新手段, 在土壤侵蝕研究中得到廣泛的應(yīng)用.
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The weathering crust eluvial type REE deposits develop widely in southern Hunan.
風(fēng)化殼淋積型稀土礦床,在湘南地區(qū)普遍發(fā)育.
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We should divide th ree kind of spiritual situation: Narrowness, selfish, healthy - individualism.
我們可以分成三種情況: 狹隘 、 自私 、 個人主義.
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The Shangzhuang apatite deposit is a low - grade apatite deposit associated with Fe, vermiculitizated biotite and REE.
上莊磷礦為一大型 低品位 磷灰石礦床,伴生有益組分有鐵 、 蛭石化黑云母及稀土元素.
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This paper determined the sulfur isotopic composition of the Mianning REE deposit, Sichuan Province , China.
分析了四川冕寧大型稀土礦床硫同位素組成.
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The REE distribution pattern of the Xihu lake is similar to that of andesite.
西湖沉積物稀土分布模式與安山巖相似.
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The Muluo REE deposit is scale deposit newly found in Pan xi region.
木洛稀土礦床是攀西地區(qū)新發(fā)現(xiàn)的中型稀土礦床,在成因上與木洛英堿正長巖密切相關(guān).
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Changes in red soil microbial biomass under different REE concentrations have been studied.
本文研究了不同稀土元素在不同濃度水平下紅壤(黃筋泥)中微生物量的變化規(guī)律.
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Rare earth element pattern is a important way of study on REE geochemistry.
稀土元素模式圖是稀土元素,地球化學(xué)研究的重要途徑.
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Depending upon certain conditions there may ornot may be f ree elect rons in semi - conductors.
半導(dǎo)體是否存在著自由電子,這取決于某些條件.
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The REE content in fluid inclusions of minerals in the leaddeposit was determined by the ICP - MS .
本文采用四極等離子質(zhì)譜儀(ICP -MS )方法測定了可可塔勒鉛鋅礦礦物流體包裹體的稀土元素含量.
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The geochemical characteristics of REE in the auriferous quartz veins indicate that the ore forming f.
含金石英脈的稀土元素地球化學(xué)特征表明成礦流體具有多源性.
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The paper presents the geochemical characteristics of trace elements, REE and oxygen isotopes of kaolin rocks.
本文主要研究了煤系高嶺巖的微量 、 稀土、氧同位素地球化學(xué)特征.
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All samples have high ICE ( incompatible element ) and REE contents showing very strong mantle metasomatism.
地幔交代作用強烈,巖石富集不相容元素,明顯高于南非及西澳克拉通者.
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