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《干旱和深度风化环境中的地球化学勘探》(Geo-chemical Exploration in Afid and Deeply Wea-thered Environments)一书由R.Cavy等人编著,于1983年出版。该书第一部分由16篇文章及九篇摘要组成。论述的主要内容是:在澳大利亚干旱及深度风化环境中如何因地制宜地将原来在潮湿地区使用的地球化学方法加以改进和使用的情况。所列举的实例是澳大利亚的U,Cu,Pb,Zn,Sn,Au和Ag矿床上的地球化学勘探第二部分探讨了对铁帽的研究和识别问题。第三部分研究了金在风化进程中的迁移,用图表说明浅成金的沉淀问题。认为在于旱地区以反象在新几内亚这样一类降雨量高的(含有硫代硫酸盐成分)环境的国家里,Cl对迁移的Ag的络合是可信的。第四部分的内容是关于He,Ra同位素及U含量在找铀矿工作中的作用。这部分从大量的实际资料说明,由于石膏、黄钾铁钒和黄铁矿捕集了镭和贱金属,
Geo-chemical Exploration in Afid and Deeply Wea-thered Environments, edited by R. Cavy et al., 1983. The first part of the book consists of 16 articles and nine abstracts. The main content of the discussion is how to improve and use the geochemical methods originally used in wet areas according to the local conditions in the arid and highly weathered environment of Australia. The examples cited are geochemical exploration on the U, Cu, Pb, Zn, Sn, Au and Ag deposits in Australia. The second part explores the research and identification of iron caps. The third part studies the migration of gold in the weathering process and illustrates the precipitation of shallow gold with graphs. It is believed that the complexation of Cl with migrating Ag is believed to be in the context of arid regions that are counterproductive in such a high rainfall (containing thiosulfate) environment as New Guinea. The fourth part is about the role of He, Ra isotopes and U content in finding a uranium mine. This section from a large number of actual data shows that due to gypsum, ferro-potassium iron and vanadium and pyrite capture of radium and base metals,