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.
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