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Discovery of diamonds in the south-western uzbekistan

机译:在乌兹别克斯坦西南部发现钻石

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The paper reports the finding of diamonds in thesouth-west of Uzbekistan in connection with unusual diamond-bearing rocks: lamprophyres and schoenkinite-porphyres formingdykes and pipes. They contain xenolites both of host rocks andsome deep set rocks unknown in the region on the surface level:ultrabasites and eclogitized gabbro. There are also chromspinelides,chromdiopside, chromium-bearing olivinge and moissanite inxenolites. The paper displays data on morphology of the diamondcrystals, their x-ray powder pattern, microphotographs(electronimages) of diamonds. It is shown that the diamond-bearing deepxenolites are related to the new non-kimberlite type of rocks—lamprophyres of a camptonite-monchikite composition and/or shoninite-porphy-rites.
机译:这篇论文报道了在乌兹别克斯坦西南部发现的钻石,这些钻石与异常的含钻石岩石有关:煌斑岩和菱镁矿-斑岩形成的堤坝和管道。它们含有表层区域中未知的母岩和一些深层凝结岩的异岩:超碱土和鳞状辉长岩。也有色松,内生辉石,含铬的橄榄石和辉石的辉石。本文显示了有关金刚石晶体的形态,其X射线粉末图样,金刚石的显微照片(电子图像)的数据。结果表明,含钻石的深部异岩与新的非金伯利岩类型的岩石有关,即一种膨润土-蒙脱石组成的斑岩和/或钠盐岩-斑岩型。

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