湘鄂西褶皱带中-新生代剥蚀特征及其构造指示:来自磷灰石裂变径迹的证据

邹耀遥; 张树林; 沈传波; 张先平; 李志强; 杨超群

doi:10.3799/dqkx.2018.611

Volume 43 Issue 6

Jun. 2018

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Article Navigation > Earth Science > 2018 > 43(6): 2007-2018

Zou Yaoyao, Zhang Shulin, Shen Chuanbo, Zhang Xianping, Li Zhiqiang, Yang Chaoqun, 2018. Western Hunan-Hubei Fold Belt Exhumation Characteristics and Its Tectonic Implication in Mesozoic-Cenozoic:Evidence from Apatite Fission Track. Earth Science, 43(6): 2007-2018. doi: 10.3799/dqkx.2018.611

Citation:

Zou Yaoyao, Zhang Shulin, Shen Chuanbo, Zhang Xianping, Li Zhiqiang, Yang Chaoqun, 2018. Western Hunan-Hubei Fold Belt Exhumation Characteristics and Its Tectonic Implication in Mesozoic-Cenozoic:Evidence from Apatite Fission Track. Earth Science, 43(6): 2007-2018. doi: 10.3799/dqkx.2018.611

Citation:

Zou Yaoyao, Zhang Shulin, Shen Chuanbo, Zhang Xianping, Li Zhiqiang, Yang Chaoqun, 2018. Western Hunan-Hubei Fold Belt Exhumation Characteristics and Its Tectonic Implication in Mesozoic-Cenozoic:Evidence from Apatite Fission Track. Earth Science, 43(6): 2007-2018. doi: 10.3799/dqkx.2018.611

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Western Hunan-Hubei Fold Belt Exhumation Characteristics and Its Tectonic Implication in Mesozoic-Cenozoic:Evidence from Apatite Fission Track

doi: 10.3799/dqkx.2018.611

Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2018-03-15
Publish Date: 2018-06-15

Abstract

Abstract

Reconstruction of the Mesozoic-Cenozoic exhumation history in western Hunan-Hubei fold belt and establishing its temporal and spatial evolution play important role in the research of intracontinental orogeny as well as the petroleum exploration in this area.Based on apatite fission track (AFT) analysis and time-temperature thermal history modeling results, this work quantitively constrains the exhumation rate and thickness of the western Hunan-Hubei fold belt.The AFT ages here range from 71 to 100 Ma.Integrating with the AFT ages from fold belt in the East Sichuan basin, all the data present a younger trend from southeast to northwest.The time-temperature thermal history since Mesozoic shows a "three-stages" feature with the turning period occurred at 115-90 Ma and 35-20 Ma.The three stages correspond well with the geological evidence and respectively indicate different deformations.The deformations are respectively orogeny during Late Jurassic-Early Cretaceous, basin formation in Late Cretaceous and tectonic uplift since Cenozoic.Yanshannian event is the main cause of the deformation.The deformation occurred earlier in the southeast and later in the northwest and the exhumation also presented a pattern being stronger in the southeast and weaker in the northwest.All the recognization during this work provides strong evidences for the deformation and evolution process of the western Hunan-Hubei to East Sichuan fold belt.
- western Hunan-Hubei fold belt,
- Mesozoic-Cenozoic,
- apatite fission track,
- thermal history modeling,
- exhumation characteristics,
- petroleum geology

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References(73)

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