“~(210)Po法”是近几年来引进的一种探测 a 粒子的铀矿普查的放射性方法。现在已有不少单位把这种方法也应用到地热区的勘探中,并取得了一定的效果。一九八三年我们与浙江水文地质队一起应用这种方法对浙江西部的湍口地热区进行工作,从所测出的结果经过分析整理后可以看出,这一方法对搞清地热区的构造情况可以起到一定作用。 The “~ (210) Po method” is a radioactive method for the uranium prospecting of a particle in recent years. At present, many units have also applied this method to the exploration of geothermal areas and have achieved certain results. In 1983, we used this method together with Zhejiang Hydrogeological Team to work on the turbulent geothermal area in the west of Zhejiang Province. From the measured results, we can see that this method is very useful for geothermal area Structure can play a role.