Detachment fault play a key role in the Lithospheric extension process.
在岩石圈伸展过程中，剥离断层起着重要的作用。
Indicate an intense degree and a long period of of the lithospheric thinning beneath the fault zone, its occurrence and activities provides an routeway and an important role to magma activities.
暗示断裂带内岩石圈具有较长的减薄历史和较强的减薄程度，断裂带的存在和活动为岩浆活动提供了良好的通道和有利的条件。
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.
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.
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。
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