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依作者见解,地壳最先的地质构造上的结构,是那些其遗迹直到今天仍保存在太平洋内部的原生矽镁地台。从太古代开始时起,原始矽镁地壳的隆起部份一直是那不连续的“花岗岩”矽铝层发展的舞台。矽铝层发展阶段的顺序,决定于这样的一个公式:大地槽阶段——今天在地形上表现为陆块形式的次生矽铝地台阶段。从太古代的开始一直到现在,大地构造作用的共同方向,表现为原生矽镁地台面积的减缩,和大陆型次生矽铝地台的扩展。
According to the authors, the first structural geological structure of the earth’s crust is that of the native magnesian magnesia whose remains are still preserved in the interior of the Pacific today. From the beginning of the Archean, the protuberance of the original magnesian crust has been the stage for the development of discontinuous “granite” Si-Al layers. The sequence of development phases of the Si-Al layers is determined by such a formula that the Trough stage - the secondary Si-Al platform stage present on the terrain today in the form of a block. From the beginning of the Archean to the present, the common direction of tectonics has been shown by the reduction of the base area of primary magnesia and the expansion of continental secondary aluminosilicate stations.