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A.Berehep根据对固体地球表面高程曲线的分析,曾预言过大洋地壳与大陆地壳间的根本差异,然而,一直过了四十年,它才被大洋的地震探测所直接证实。在现代,大规模的深海钻探和在大洋中脊裂谷带、海沟壁、转换断层崖壁所从事的大规模拖挖取样,以及对采集物的岩石学和地球化学(包括同位素)分析,对于以下两点不再有更多的疑问了:一是大洋地壳显著不同于大陆地壳,二是大洋地壳并不带有大陆地壳被同化的任何微小痕迹。大洋壳和大陆壳之间的差
A.Berehep predicted the fundamental difference between the oceanic crust and the continental crust on the basis of an analysis of the elevation curve of the solid Earth’s surface. However, it has been 40 years since it was directly confirmed by oceanic seismic surveys. In modern, large-scale deep-sea drilling and large-scale drag-and-dig sampling of the mid-oceanic ridges and rift belts, trench walls, transgressive cliffs, and petrological and geochemical (including isotopic) analyzes of the collected materials, The following two points no longer have more questions: First, the oceanic crust is significantly different from the continental crust, and second, the oceanic crust does not contain any tiny traces of the assimilation of the continental crust. The difference between the oceanic crust and the continental crust