大别造山带中元古代变沉积岩碎屑锆石U-Pb年代学与Hf同位素特征及其地质意义

孔令耀; 郭盼; 万俊; 刘成新; 王晶; 陈超

doi:10.3799/dqkx.2021.096

Volume 47 Issue 4

Apr. 2022

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Article Navigation > Earth Science > 2022 > 47(4): 1333-1348

Kong Lingyao, Guo Pan, Wan Jun, Liu Chengxin, Wang Jing, Chen Chao, 2022. Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance. Earth Science, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096

Citation:

Kong Lingyao, Guo Pan, Wan Jun, Liu Chengxin, Wang Jing, Chen Chao, 2022. Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance. Earth Science, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096

Citation:

Kong Lingyao, Guo Pan, Wan Jun, Liu Chengxin, Wang Jing, Chen Chao, 2022. Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance. Earth Science, 47(4): 1333-1348. doi: 10.3799/dqkx.2021.096

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Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance

doi: 10.3799/dqkx.2021.096

Kong Lingyao^{1, 2
,
,},
Guo Pan^{1, 2},
Wan Jun^{1, 2},
Liu Chengxin^{1, 2},
Wang Jing³,
Chen Chao^{1, 2}

1.
Hubei Geological Survey, Wuhan 430034, China
2.
Hubei Research Center of Geological Exploration and Engineering Technology, Wuhan 430034, China
3.
Wuhan Center of China Geological Survey, Wuhan 430205, China

Received Date: 2021-05-11
Available Online: 2022-04-29
Publish Date: 2022-04-25

Abstract

Abstract

The Dabie orogen is located in the north margin of the Yangtze block. Recent studies show that the Dabie orogen has Archean-Paleoproterozoic crystalline base, but it has been lack of Mesoproterozoic material information all the time. In this article, it reports a set of Mesoproterozoic sedimentary rocks mainly composed of "metasandstone-marble" in the Dabie orogen for the first time. It analyzes the detrital zircon U-Pb chronology and Lu-Hf isotopic characteristics of the three samples in this strata, and the results show that the youngest average ages of three samples are: 1 556±13 Ma, 1 541±20 Ma and 1 584.3±24 Ma. This three ages are basically same within the error-range, which shows that the age of this strata should be the Mesoproterozoic. The metamorphic rims of detrital zircon record a metamorphic event at the age of 124.1±2.3 Ma, the U-Pb age histograms and Lu-Hf isotopes shows that the provenance characteristics of this strata are consistent with the Shennongjia Group. The main peaks of detrital zircon U-Pb ages of 2 682 Ma and 2 461 Ma record two important growth events of Dabie crystalline basement, and the peaks of 2 043 Ma, 1 803 Ma, 1 572 Ma implicate that the "Dabie block" may have participated in the aggregate event of Columbia supercontinent and become a part of it, and the "Dabie block" separated from the Columbia supercontinent during the breaking up event, and collided with the "Huangling continental nucleus" and became an important part of the basement of the Yangtze block during the Early Neoproterozoic.
- Dabie orogen,
- Dabie Group-complex,
- Mesoproterozoic metasedimentary rock,
- detrital zircon,
- U-Pb geochronology,
- Lu-Hf isotope,
- stratigraphy

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References(84)

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Detrital Zircon U-Pb Geochronology and Hf Isotopes of Mesoproterozoic Metasedimentary Rocks in Dabie Orogen and Its Geological Significance

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