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THE BEHAVIOUR OF SELENIUM IN GEOLOGICAL PROCESSES

机译:硒在地质过程中的行为

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Selenium contents were analysed from a total of 244 soil samples collected over dif- ferent rock types at a sampling density of one sample per 4 km~2 around Geita gold mining areas, Northwestern Tanzania. Comparisons using literature survey contents of selenium in geological ma- terials and some implications on the selenium in soils are compiled and discussed. Most selenium occurs as simple selenides in small quantities in low temperature hydrothermal deposits devoid of sulphur. It has been observed that to a large extent selenium content is increased more than most trace elements in the upper parts of the Earth perhaps through extraterrestrial deposition.
机译:在坦桑尼亚西北部的吉塔金矿区附近,从总共244种不同岩石类型中收集的硒含量进行了分析,采样密度为每4 km〜2 1个样品。汇编和讨论了使用文献资料中地质物质中硒的比较进行的比较,以及对土壤中硒的一些影响。大多数硒以简单的硒化物形式出现在不含硫的低温热液矿床中。已经观察到,硒的含量增加的程度可能比地球上部的大多数微量元素高,这可能是由于地球外的沉积所致。

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