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宁强陨石的岩石学、岩石化学及基质的化学成份。Petrology, petrologic Chemistry, and Matrix Chemical Compositions of the Ningqiang Chondrite.

过渡元素球粒陨石标准化曲线,也均呈微向右倾斜的W形曲线。The transitional element curves standardized by chondrite were all W type curves inclining gently to the right.

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并与先前肇东陨石全岩样的高压熔融实验进行比较。The metal-sulfide phase of previous melting experimental results of Zhaodong chondrite was observed and analysed again.

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

通过模糊聚类分析和因子分析讨论了元素间的相关关系。Relations among the element concentrations for chondrules from the Boxian chondrite are discussed using the clustering and factor analysis.

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

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

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

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

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。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.

对福建省钟腾花岗岩体不同阶段岩石中锆石的物理—化学性质、稀土元素组成及球粒陨石模式、红外光谱特征进行了研究。Physical-chemical properties, REE compositions, chondrite pattern and infra-red spectrum characteristics of the zircon from the Zhongteng intrusive of different stages in Fujian have been studied.