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Discovery of diamonds in the south-western uzbekistan

机译:乌兹别克斯坦西南部发现钻石

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摘要

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:本文报告了乌兹别克斯坦西部的钻石与不寻常的钻石岩石:林普罗斯和施洛基岩 - 卟啉矿床和管道。 它们含有Xenolites在地表水平的区域内未知的主体岩石和组织深度岩石:超级岩石和eClogitized Gabbro。 还有酚膦酸,铬透明剂,含铬的橄榄油和Moossanite Inxenolites。 本文显示了Diamondrystals的形态数据,钻石的X射线粉末图案,微镜(电动因子)的数据。 结果表明,含有菱形的深蛋白与Campptonite-Monchikite组合物和/或Shoninite-Zorphy-Rites的新的非金伯利岩岩石晶体相关。

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