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Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance
Li Puqing, Song Dongfang, Zeng Hao
PDF(7428 KB)
PDF(7428 KB)
Provenance Characteristic of Devonian Chaganhabu Formation in the Northern Margin of the North China Craton and Its Tectonic Significance
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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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感谢两位审稿人提出的宝贵意见和编辑部老师的辛勤付出！
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