华北北缘泥盆纪查干哈布组物源特征及其构造意义

李普庆; 宋东方; 曾浩

doi:10.3799/dqkx.2022.056

Volume 48 Issue 3

Mar. 2023

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Li Puqing, Song Dongfang, Zeng Hao, 2023. Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance. Earth Science, 48(3): 1205-1216. doi: 10.3799/dqkx.2022.056

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Li Puqing, Song Dongfang, Zeng Hao, 2023. Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance. Earth Science, 48(3): 1205-1216. doi: 10.3799/dqkx.2022.056

Citation:

Li Puqing, Song Dongfang, Zeng Hao, 2023. Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance. Earth Science, 48(3): 1205-1216. doi: 10.3799/dqkx.2022.056

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Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance

doi: 10.3799/dqkx.2022.056

Li Puqing^{1, 2, 3
,
,},
Song Dongfang^{1, 2, 3
,
,
,},
Zeng Hao^{1, 2, 3}

1.
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2.
Innovation Academy for Earth Science, CAS, Beijing 100029, China
3.
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2022-01-28
Available Online: 2023-03-27
Publish Date: 2023-03-25

Abstract

Abstract

The Bainaimiao arc belt is located in the northern margin of the North China Craton. The exact time of the collision between the Bainaimiao arc belt and the North China Craton is thus a key for understanding the accretionary process of the northern margin of the North China Craton. In order to constrain the collision time of the Bainaimiao arc belt and the North China Craton, this study carried out zircon U-Pb age dating and zircon Lu-Hf isotope analysis of the Chaganhabu Formation. The weighted average age of the three youngest zircons from the Chaganhabu Formation is 393.5±4.9 Ma, consistent with previous paleontological reports. Therefore, the maximum deposition age of the Chaganhabu Formation is the late Early Devonian. Moreover, the characteristic of zircon U-Pb age spectra and Hf isotope of the Chaganhabu Formation is similar to that of the Bainaimiao arc belt and different from that of the North China Craton, which means that the provenance of the Chaganhabu Formation is the Bainaimiao arc belt rather than the North China Craton. Combined with regional tectonic research, these data indicate that during the Early Devonian, there was still a wide ocean between the Bainaimiao arc belt and the northern margin of the North China Craton, and the arc-continent collision has not yet occurred.
- Bainaimiao arc belt,
- Chaganhabu Formation,
- zircon U-Pb age,
- zircon Hf isotope,
- provenance characteristic,
- tectonics

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References(55)

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Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance

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