本文是叙述为寻找金属矿床运用野外水化学调查方法的审查结果,这种方法是由全苏水文地质及工程地质研究所的专家们集体拟定的。野外水化学方法的调查工作是在一个地质队里,与其他类型的普查工作综合进行的,调查面积包括走向为西北的山麓部分,最大标高达2500公尺。在这个区域矿产远景地段的地质结构主要是始新世的凝灰岩,其剖面如下(由老到新):1.主要为辉石玢岩,局部过渡为凝灰岩的下部喷发凝灰岩层,厚度为300公尺。2.下部为凝灰岩,顺剖面向上过渡为簿层凝灰砂 This article describes the results of a review of the field water chemistry investigations used in the search for metallogenic deposits developed by experts from the Institute of Hydrogeology and Engineering Geology in Quanzhou. Investigations of field water chemistry methods are conducted in a geologic team integrated with other types of census work, covering an area of ​​up to 2,500 meters up to the foothills of the northwest. The geological structure of the foreground prospect in this area is dominated by Eocene tuffs, which are profiled (from old to new) as follows: 1. The predominantly pyroxene rock, locally transiting to the lower tuff, is an eruptive tuff layer 300 m thick. 2. The lower part of the tuff, along the profile of the transition layer tuff sand