• The Allende meteorite is classified as a chondrite.

    阿连德陨石被归类为球粒陨石。

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  • This, too, is the case for the ordinary-and carbonaceous-chondrite groups.

    而对普通陨石和碳质球粒陨石也都是如此。

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  • The chondrite-normalized patterns of rare earth elements are in seagull forms.

    稀土元素配分模式呈海鸥型。

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  • The standard curve of chondrite of rare earth element reveals a deficit of light rare earth enriched the heavy one;

    稀土元素球粒陨石标准化曲线显示轻稀土富集重稀土亏损;

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  • Carbonaceous chondrite planetesimals were adsorbed on the mantle surface of the primitive earth, forming primitive carbon-rich areas.

    碳质球粒陨石星子被吸积于原始地球上地幔表层,形成原始富碳区。

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  • Relations among the element concentrations for chondrules from the Boxian chondrite are discussed using the clustering and factor analysis.

    通过模糊聚类分析和因子分析讨论了元素间的相关关系。

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  • Only one ore sample is compositionally close to mantle inclusion, chondrite mantle or komatiite, indicating the property of deep mantle source.

    仅有一件矿石样品与地幔包体、球粒陨石地幔或科马提岩接近,暗示其深部地幔源区的性质。

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  • The chemical compositions of the Ningqiang carbonaceous chondrite matrix and a dark rim are analysed with instrumental neutron activation method.

    采用仪器中子活化方法分析了宁强碳质球粒陨石基质及暗色边化学成份。

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  • The lithophile elements in ordinary and carbonaceous chondrite groups may display either chalcophile or siderophile nature in enstatite chondrites.

    普通球粒陨石和碳质球粒陨石中的亲石元素在顽火辉石球粒陨石内显示亲铜或亲铁的性质。

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  • The REE content and chondrite nomalized patterns of the altered and mineralized rocks are largely consistent with those of the unaltered host rocks.

    不同蚀变与矿化岩石的稀土含量和配分模式与未蚀变泥质灰岩基本一致。

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  • The average composition for our sample is different in some ways from the CI chondrite meteorites: namely we found more zinc, gallium, and copper, and less sulfur.

    我们样品的平均成分水平在某些方面与CI球粒陨石不同:即我们发现有较多的锌、镓和铜及较少的硫。

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  • The large number of meteorites from Antarctica and the desert areas of Australia, Africa and North America changed the previous chondrite classification in recent years.

    近年来在南极及澳大利亚、非洲和北美的沙漠地区发现和回收了大量的陨石,改变了以前的球粒陨石分类。

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  • The Lujiang meteorite, a chondrite whose petrochemical type is LL6, contains the following opaque minerals: kamacite, taenite, disordered taenite, troilite, chromite, hematite, ilmenite. etc.

    庐江陨石是一化学岩石类型为LL6的球粒石陨石。研究表明该陨石中不透明矿物有铁纹石、镍纹石、陨硫铁、铬铁矿、钛铁矿和赤铁矿等。

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  • Petrology, petrologic Chemistry, and Matrix Chemical Compositions of the Ningqiang Chondrite.

    宁强陨石的岩石学、岩石化学及基质的化学成份。

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  • Petrology, petrologic Chemistry, and Matrix Chemical Compositions of the Ningqiang Chondrite.

    宁强陨石的岩石学、岩石化学及基质的化学成份。

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