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本文作者试图利用统计学的可能性,在研究作为岩浆作用指示剂的放射性元素分布情况的基础上,再用地球化学方法对地层进行划分作了探讨。选择了地质方面研究得相当详细的哈萨克斯坦中部的花岗岩侵入体——克耳查和库乌作为研究的对象。为了同已获得的成果进行对比,曾参照了许多由K.K.日洛夫同志结我们大力提供的有关舍特地区岩体的研究资料。根据现有的地质资料,这些与海西宁岩浆活动有关的侵入岩广泛地分布于哈萨克斯坦中部范围内。其中可分成两种花岗岩类:1)海西宁早期的主要
The authors attempt to use the possibility of statistics to study the distribution of radioactive elements as indicators of magmatic activity and to discuss the stratigraphic division by geochemical methods. The geologically studied granite intrusions, which are quite well-studied in central Kazakhstan, are Kerr and Kuau. In contrast to the achievements already obtained, many references have been made to Comrade K. K. Zilov, who volunteered us to provide information on the study of the rock mass in the Hutt area. According to the existing geological data, these intrusive rocks related to the Hercynian magmatism are widely distributed in the central region of Kazakhstan. Which can be divided into two types of granite: 1) Hercynian early major