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Coupling and transition of Meso-Cenozoic intracontinental deformation between the Taihang and Qinling Mountains
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d="p0005">The transition of compression to extension in East China is in late Early Cretaceous.

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d="p0010">The transition is caused by the collision to the west and the subduction to the east.

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d="p0015">The transition of the two tectonic belts is related to lithospheric heterogeneity.

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d="p0020">Intraplate extension is characterized by diffuse multi-directional cracking.

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d="p0025">Differential deformation is controlled by preexisting tectonic pattern in basements.

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