| Citation: | Jiazhen Sun, Xianghua Yang, Ronghua Qiu, Mingxi He. Dynamic Settings and Interactions between Basin Subsidence and Orogeny in Zhoukou Depression and Dabie Orogenic Belt. Journal of Earth Science, 2000, 11(3): 369-371.
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This paper presents a study of the geo-dynamic setting and the relation between orogenic uplift and basin subsidence in the inland Zhoukou depression and Dabie orogenic belt.Since the Mesozoic the evolution of Zhoukou depression can be divided into three stages: (1) foreland basin, (2) transitional stage, (3) fault depression.Formation and variations of basin were not only related to the orogenesis, but also consistent with the orogenic uplift.
| Stockmal G S, Christopher B, Boutilier R, 1986. Geodynamic Models of Convergent Margin Tectonics: Transition from Rifted Margin to Overthrust Belt and Consequence for Foreland Basin Development. AAPG, 70(2) : 181-191 |
| Liu D, Li S, Peng Z, 1990. The Discovery of Supermylonite Vein and Geological Significence in Dabie Mountain. Scientia Geological Forum, 183-185 |
| Pang G, 1993. Volcanism of Dabie Orogenic Collision Belt, in Volcanism of Volcanic Rocks and the Associated Minerals. Geological Review, 39: 45-51 |
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