鄂西中央背斜带中生代构造演化过程:来自磷灰石裂变径迹的证据

李朋; 胡正祥; 何仁亮; 李雄伟; 吴龙; 宗维; 杜小锋; 周峰

doi:10.3799/dqkx.2018.517

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2518-2526

Li Peng, Hu Zhengxiang, He Renliang, Li Xiongwei, Wu Long, Zong Wei, Du Xiaofeng, Zhou Feng, 2018. The Tectonic Evolution of the Central Anticline in Western Hubei of China during Mesozoic: Evidences from Apatite Fission Track. Earth Science, 43(7): 2518-2526. doi: 10.3799/dqkx.2018.517

Citation:

Li Peng, Hu Zhengxiang, He Renliang, Li Xiongwei, Wu Long, Zong Wei, Du Xiaofeng, Zhou Feng, 2018. The Tectonic Evolution of the Central Anticline in Western Hubei of China during Mesozoic: Evidences from Apatite Fission Track. Earth Science, 43(7): 2518-2526. doi: 10.3799/dqkx.2018.517

Citation:

Li Peng, Hu Zhengxiang, He Renliang, Li Xiongwei, Wu Long, Zong Wei, Du Xiaofeng, Zhou Feng, 2018. The Tectonic Evolution of the Central Anticline in Western Hubei of China during Mesozoic: Evidences from Apatite Fission Track. Earth Science, 43(7): 2518-2526. doi: 10.3799/dqkx.2018.517

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The Tectonic Evolution of the Central Anticline in Western Hubei of China during Mesozoic: Evidences from Apatite Fission Track

doi: 10.3799/dqkx.2018.517

Hubei Geological Survey, Wuhan 430034, China

Received Date: 2018-01-11
Publish Date: 2018-07-15

Abstract

Abstract

The central anticline of the western Hubei is located in the tectonic zone of the Yangtze block and the central Sichuan (western Hubei) foreland basin, which possesses important advantages for the study of regional tectonic evolution. In this paper, according to the detailed field geological survey and evidences form apatite fission track simulation, five stages of tectonic activities have been identified:(1) tectonic uplift at 187.4 Ma-180.1 Ma that resulted in the parallel unconformity between the Jiuligang Formation and the Tongzhuyuan Formation. (2) tectonic subsidence and deposition of terrestrial sediments at 180.1 Ma-115.6 Ma. (3) slowl tectonic uplift once again associated with land erosion during 115.6 Ma-78.8 Ma. (4) subsidence again and the deposition of Cretaceous Paomagang Formation during the period of 78.8 Ma-63.6 Ma. (5) followed by great uplift until a small subsidence at 2.6 Ma of the Quaternary. Based on the tectonic evolution and the application of balanced profile technology, the regional tectonic pattern of extrusion-stretching process was established.
- tectonic evolution,
- fission track,
- balanced cross-section,
- Mesozoic,
- western Hubei,
- geochronology

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References(28)

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The Tectonic Evolution of the Central Anticline in Western Hubei of China during Mesozoic: Evidences from Apatite Fission Track

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