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为了解决铜-镍矿床矿体成因和起源的一系列问题,有必要在上地幔及其岩浆衍生物的硫化物矿化作用研究方面进行专门工作。根据大多数研究者的意见,金伯利岩中的深部捕虏体(深源包体)可作为提供上地幔物质状态特点的样品。迄今为止,文献中已积累了说明这些深源包体的硫化物矿化作用的大量实际材料,这就可将我们所获得的资料与之进行对比,从而得到硫化物的较全面的特征。由于要解决上地幔的结构和成分问题,金伯利岩深部捕虏体岩石学方面的研究得到了广
In order to solve a series of problems of genesis and origin of copper-nickel orebodies, it is necessary to do some special work in the research of sulfide mineralization of upper mantle and its magma derivatives. According to most researchers, the deep xenoliths (deep-core inclusions) in the kimberlite can be used as samples to characterize the material condition of the upper mantle. So far, a great deal of practical material has been accumulated in the literature that illustrates the sulphide mineralization of these deep-sourced inclusions, which allows us to compare the data we have obtained with them to obtain a more comprehensive picture of sulphides. Due to the structural and compositional problems of the upper mantle, the study of deep xenoliths in the kimberlite has been extensively studied