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铂族矿物中Os—Ir—Ru三元系的端员矿物自然钌发现于我国广东省阳春县南湖大墩岭超基性岩体中。1976年初,根据电子探针资料作过初步定名,并先后在内部发行的《广东阳春县南湖大墩岭含铂超基性岩体氧化带中的铂钯赋存状态研究》及《广东地质实验情报》(1978年第四期)作过初步报导。自1978年起,我们继续对该矿物作深入研究,重新测定了成分和其它物理性质,并在武汉地质学院彭志忠教授帮助和指导下作了X射线分析。自然钌在矿物学研究方面又进了一步。
The natural ruthenium of terminal mineral of the Os-Ir-Ru ternary system in the platinum group minerals was found in the Dadunling ultrabasic rock mass of Nanhu Lake, Yangchun County, Guangdong Province, China. In early 1976, based on the electronic probe data, it was initially named and published successively in “The State of Platinum and Palladium in the Oxidation Belt of Dadunling Poyangdian, Yangchun County, Guangdong Province” and “Guangdong Geological Experiment Intelligence ”(1978 fourth issue) made a preliminary report. Since 1978, we continue to study the mineral in depth, re-measured the composition and other physical properties, and conducted X-ray analysis with the help and guidance of Professor Peng Zhizhong from Wuhan Institute of Geology. Natural ruthenium has taken another step in mineralogy.