板块构造体系说明洋壳俯冲极性从南向北。
The plate tectonic regime suggests the subduction sense from south to north.
本区不存在现代板块构造体系，而具有多旋回海槽(盆)的活动形式。
There is not the contemporary plate-tectonic system in the researching area. However, the active forms of polycycle trough (basin) developed in the area.
星球级纬向构造体系是控制板块边界和运动的重要的支配力量之一。
The global latitudinal tectonic system is one of the important forces controlling the plate boundary and movement.
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