苏鲁造山带东段新生代两阶段剥露事件的磷灰石(U-Th)/He热年代学证据

林旭; 吴林; MarcJolivet; 李长安; 刘海金

doi:10.3799/dqkx.2021.083

Volume 47 Issue 4

Apr. 2022

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Article Navigation > Earth Science > 2022 > 47(4): 1162-1176

Lin Xu, Wu Lin, Marc Jolivet, Li Chang’an, Liu Haijin, 2022. Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt. Earth Science, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083

Citation:

Lin Xu, Wu Lin, Marc Jolivet, Li Chang’an, Liu Haijin, 2022. Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt. Earth Science, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083

Citation:

Lin Xu, Wu Lin, Marc Jolivet, Li Chang’an, Liu Haijin, 2022. Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt. Earth Science, 47(4): 1162-1176. doi: 10.3799/dqkx.2021.083

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Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt

doi: 10.3799/dqkx.2021.083

Lin Xu^{1, 2, 3
,
,},
Wu Lin²,
Marc Jolivet⁴,
Li Chang’an^{3
,
,},
Liu Haijin⁵

1.
School of Civil Engineering and Architecture, China Three Gorges University, Yichang 276005, China
2.
Ar-Ar and (U-Th)/He Geochronology Laboratory, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
3.
School of Geography and Information Engineering, China University of Geosciences, Wuhan 430078, China
4.
Faculty of Earth Sciences, France University Ⅰ Rennes, Rennes 35042, France
5.
School of Earth Sciences, East China Institute of Technology, Nanchang 330013, China

Received Date: 2021-02-16
Available Online: 2022-04-29
Publish Date: 2022-04-25

Abstract

Abstract

The Sulu orogenic belt, located between the North China and South China plates, is one of the most prominent intracontinental orogenic belt in eastern China. Therefore, the denudation history of Sulu orogenic belt provides significant insight into the basin-mountain evolution in eastern China and their dynamic mechanism. Due to the apatite (U-Th)/He system has low closure temperature (ca. 70 ℃), it can constrain the cooling processes of geological bodies more accurately in the upper crust. In this study, the apatite (U-Th)/He method was used to analyze the exhumation time of rocks on the Duofu and Juchi mountains located in the eastern parts of Sulu orogenic belt. The apatite (U-Th)/He age-elevation relationship and thermal history simulation results show that the exhumation occurred in the Early-Middle Eocene (54-43 Ma) and Oligocene (35-27 Ma) for the Duofu and Juchi mountains, respectively. These cooling episodes were synchronized with the exhumation time of the western part of the Sulu orogenic belt. Combined with the results reported in the region, it is shown that the eastern China was influenced by the Pacific and Indian plates subduction into Eurasia, and the extensive exhumation process occurred in the Early Cenozoic, which established the basin-mountain distribution pattern during this time.
- Sulu orogenic belt,
- apatite uplift,
- (U-Th)/He thermochronology,
- tectonics,

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致谢: 衷心感谢两位审稿人的修改建议以及对文稿的仔细修改.

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Apatite (U-Th)/He Thermochronology Evidence for Two Cenozoic Denudation Events in Eastern Part of Sulu Orogenic Belt

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