燕山期，全面陆-陆碰撞期间其主要表现为脆性变形特征。
The brittle deformation mainly occurred in the nouthern part during continent-continent collision in the Yanshanian epoch.
摘要：亚特拉斯山和阿特拉斯山是与已存在和仍在发育的陆-陆碰撞相连的褶皱带。
The High Atlas and the Anti Atlas are fold-belts linked to former and still ongoing continent–continent collisions.
东准噶尔双泉一带的韧-脆性剪切带是在板块结合带基础上，形成于陆-陆碰撞体制。
Basing on the combination of plates, ductile-brittle shear zone in the ShuangQuan area, Eastern JungGar forms in the system of continental - continental collision.
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