硅铝层

硅铝层深部地壳形变去除了外壳或褐色外层。

Having husk or outer brown layers removed .

硅铝层深部地壳形变地球的外壳是分层的。

The earth 's crust is layered .

它们很可能是由地壳硅铝层重熔的花岗岩浆经结晶分异作用而形成的。

It is most possible that the massifs are of magmatic origin from fractional crystallization of crust-remelted granitic magma .

福建东南沿海断裂1多发生于上地壳硅铝层，少数达硅镁层。

Most of the faults in the southeast coast of Fujian Province occur in the sial of upper crust and some have reached the sima .

根据现代地质学、地球物理学和岩石地球化学多学科的综合分析，将弧后盆地划分为五种成因类型：（1）弧后硅铝层上裂陷盆地；

Based upon the multiple disciplinary studies of earth sciences , the back arc basins might be divided into five genetic types : ( 1 ) back arc ensialic taphrogenic basin ;

直流电磁场下铝硅-铝镁复层材料的制备

The Process for Clad Metal of Al-Si and Al-Mg under Direct Electromagnetic Field

430不锈钢热浸镀铝（硅）之铝化层成长研究

The Growth of Aluminide-layer during the Hot-dipping Al - ( Si ) Coating onto 430 Stainless Steels