PALEOPROTEROZOIC CRUST-SCALE TRANSTE 中国北部古元古代地壳尺度的伸展拆离和硅铝壳内活动带
LARGE-SCALE NE-TRENDING CRUST-BLOCK-SLIP OBL 斜切中亚的大规模北东向地壳块体滑移
Mantle material can sink at a plate boundary, and then flow back upward farther away, pushing on the crust - a process called small scale convection.
地幔，这种物质可以在板块边界处下沉，然后向上回流到较远的地方，再与地壳相碰撞——这个过程被称为小规模的对流。
The long-term tectonic activity formed a series of great scale active faults that divided plateau crust into blocks in different size and shape.
长期的构造活动形成了一系列规模宏大的活动断裂，这些不同性质的断裂又将高原地壳切割成大小不同、形状各异的活动地块。
The elevation of crust can make rock gold deposit weather and denude and the level of the denudation depends on the scale of the elevation.
地壳上升会使岩金矿床风化剥蚀，而剥蚀程度取决于地壳上升幅度。
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