Coupling and transition of Meso-Cenozoic intracontinental deformation between the Taihang and Qinling Mountains
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- 作者：Sanzhong Lia ; b ; sanzhong@ouc.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Lingli Guoa ; b ; Liqing Xua ; b ; Ian D. Somervillec ; Xianzhi Caoa ; b ; Shan Yua ; b ; Pengcheng Wanga ; b ; Yanhui Suoa ; b ; Xin Liua ; b ; Shujuan Zhaoa ; b
- 关键词：Taihang Mountains Tectonic Belt ; The Qinling Orogenic Belt ; Intraplate deformation ; Thrust and nappe tectonics ; Intracontinental orogeny ; Tectonic regime
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：15 December 2015
- 年：2015
- 卷：114
- 期：part_P1
- 页码：188-202
- 全文大小：9242 K
文摘
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The transition of compression to extension in East China is in late Early Cretaceous.
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The transition is caused by the collision to the west and the subduction to the east.
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The transition of the two tectonic belts is related to lithospheric heterogeneity.
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Intraplate extension is characterized by diffuse multi-directional cracking.
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Differential deformation is controlled by preexisting tectonic pattern in basements.