Active Continental Margins 活动大陆边缘
passive continental margins 被动大陆边缘
sheared continental margins 剪切型大陆边
convergent continental margins 聚敛大陆边缘
active type continental margins 活跃型大陆边缘
The coarse sediments have generally accumulated along the continental margins.
粗粒沉积物一般沿大陆边缘堆积。
Detachment models can also applied to the formation of passive continental margins.
伸展区剥离断层模式同样适用于被动大陆边缘的形成和演化。
The Cenozoic basins of different magnitudes in East Asia continental margins are similar and self similar in shape.
东亚陆缘新生代盆地几何特征具有相似性,呈以nne、NEE至EW向断裂为边界的准菱形。
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