伯拉格(Berlage)提出的月球成因的增生模型与现代空间研究结果是一致的。它为地壳的地球化学演化提供了一个新的起点,在宇宙形成过程中获得的一种袋状似的卫星物质。这种袋状基性物质可能在地球地球化学史(持续了大约500百万年)的早期阶段转变成地球的硅铝壳。在下一个阶段, The hyperplastic model of lunar origin proposed by Berlage is consistent with the results of modern space research. It provides a new starting point for the geochemical evolution of the crust and a pouch-like satellite material obtained during the formation of the universe. This pocket-like matrix may have transformed into the Earth’s Si-Al shell in the early stages of Earth’s geochemistry (which lasted for about 500 million years). In the next stage,