世界文献对于元素、尤其是金属元素能从地壳深部升浮至地表的记载已有数十年了。如60年代劳特巴赫教授(卡尔·马克思大学)将铊的浓缩物置于数公里深处的土层中用来测绘其上的断裂带;80年代,苏联科学院卢卡绍夫教授也进行了以特殊吸附剂吸收游动金属元素的工作。但这些以及其它一些记载都是以由水将元素携带至地表的假设为基础的。 The world literature has for decades documented the uplift of elements, especially metallic elements, from the deep crust to the surface. For example, Professor Lauterbach (Karl Marx University) in the 1960s put the thallium concentrate in a depth of several kilometers and used it to map the faults above it. In the 1980s, Prof. Lukasoft, Soviet Academy of Sciences, Special adsorbent absorbs swimming metal elements of work. But these and other records are based on the assumption that water carries elements to the surface.