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苏联学者,如费尔斯曼(1955)把坡缕石称为俄罗斯矿物,因为早在18世纪初就把这种矿物描述为山软皮和山软木,主要与石棉有关。直到1860年,当在Perm省Popovka河附近的坡缕哥斯克(Palygorsk)矿区勘探山软皮矿床时,把这种稀有矿物推想为一种石棉的变种来加以描述。这种互相交织的纤维状矿物的原始描述表明了它含铝较高,依该矿床的产地而得名“坡缕石”,并把它作为一种新的矿物族。这种铝/镁含水硅酸盐矿物族的独特性质与石棉族矿物有着本质的差别,这种差别被后来在伏尔加附近发现的相似物质的描述所证实。
Soviet scholars, such as Felssman (1955), called palygorskite a Russian mineral because it was described as a mountain of softwood and mountain softwood as early as the early eighteenth century, primarily asbestos. It was not until 1860 when a mountain of soft-skin deposits was explored at the Palygorsk deposit near the Popovka River in Perm province that this rare mineral was assumed to be a variant of asbestos. The original description of this intertwined fibrous mineral shows that it is high in aluminum and is named “palygorskite” according to the origin of the deposit and uses it as a new mineral group. The unique nature of this aluminum / magnesium hydrous silicate mineral family is essentially different from that of asbestos minerals, as evidenced by the subsequent description of similar materials found near Volga.