断裂带在晚白垩世-早第三纪的伸展活动中，软流圈进行了强烈的上隆，岩石圈出现了显著的细颈化，属于纯剪切伸展模式。
During extensional activities of Late Cretaceo us to Eogene, intense upwelling of asthenosphere happened under the fault zone, leading to lithospheric necking in pure shear mode1.
这些银色的线围着夜色里黑暗的地球伸展，创造出一个引人注目的蜘蛛网，显示出我们全球扩张的模式。
These silvery threads stretching around the dark globe create a dramatic spider's web showing the patterns of our global sprawl.
该模式为揭示伸展构造系统中复杂断层组合之间的内在联系提供了新的思路。
This model provides a new idea for revealing the internal relationships of complicated fault assemblages in an extensional tectonic system.
本次工作所发现的弧后大陆边缘伸展方向和大洋板块运动方向相吻合，支持弧后拉张机制应为板片后退模式。
The coupling relation between the directions of the overriding plate extension and oceanic plate motion supports the slab rollback model for the back-arc extension.
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。
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。
Detachment models can also applied to the formation of passive continental margins.
应用推荐