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1)  mafic-ultramafic complex
镁铁-超镁铁杂岩
2)  ultramafic complex
超镁铁杂岩
1.
Geochemical Pt and Pd exploration led to the discovery of two precious metal anomalous concentrations in the Gaositai ultramafic complex,Hebei Province.
在高寺台超镁铁杂岩体发现了2种铂族元素异常:一种异常分布在杂岩体纯橄榄岩或橄榄岩带的镁质超基性岩中,与已知的含铂族铬铁矿有关,与已知的铬、钴、镍等矿化主金属的强异常密切共生。
3)  Post-collisional mafic-ultramafic complex
碰撞后镁铁-超镁铁杂岩
4)  mafic-ultramafic intrusions
镁铁超镁铁质杂岩体
5)  ultramafic complex
超镁铁杂岩体
1.
Geochemical constraints on petrogenesis of Hashatubei ultramafic complex, Inner Mongolia.;
内蒙古哈沙图北超镁铁杂岩体成因的地球化学制约
6)  ultramafic rock
超镁铁岩
1.
Mafic-ultramafic rock association and the mineralization-forming specialization of Cr-Ni deposit;
镁铁-超镁铁岩的自然组合与铬镍矿床的成矿专属性
2.
Based on the occurrence of Dongchinling shonshugou ultramafic rock and the characteristics of the chromite mineralization as well as the mineral components, a comprehensive explanation of the mineralization characteristics of the various chromites, such as those of being as the accessory minerals and those of different types of ore, has been proposed through the analyses of Mssbaur spectra.
以东秦岭松树沟超镁铁岩体的产状和铬铁矿的产出特征为背景,结合铬铁矿的组分特征,对副矿物铬铁矿和不同矿石类型铬铁矿的穆斯堡尔谱进行成矿特征方面的解释;并通过与铬铁矿形成有关的宏观和微观地质现象分析,指出铬铁矿体是地幔岩高度熔融形成的富铬和镁的极端部分。
3.
On the basis of summarizing former relative works, this paper manily discusses the PGE distribution in ultramafic rock and the behaviour during partial melting, crystal frac-tionation, and alteration.
在总结前人工作的基础上,论述了PGE在超镁铁岩中的分布范围以及在部分熔融、结晶分异和蚀变作用过程中的行为规律。
补充资料:钨铁电炉出铁(吉林铁合金厂)


钨铁电炉出铁(吉林铁合金厂)


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