华北克拉通东缘新元古代早期基性岩床的时代及其地质意义：来自锆石学的证据

孙逊; 刘超辉; 段瑞涵

doi:10.3799/dqkx.2023.095

Volume 49 Issue 9

Sep. 2024

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Article Navigation > Earth Science > 2024 > 49(9): 3122-3139

Sun Xun, Liu Chaohui, Duan Ruihan, 2024. The Age and Geological Significance of Early Neoproterozoic Mafic Sills on the Eastern Margin of the North China Craton: Evidence from Zirconology. Earth Science, 49(9): 3122-3139. doi: 10.3799/dqkx.2023.095

Citation:

Sun Xun, Liu Chaohui, Duan Ruihan, 2024. The Age and Geological Significance of Early Neoproterozoic Mafic Sills on the Eastern Margin of the North China Craton: Evidence from Zirconology. Earth Science, 49(9): 3122-3139. doi: 10.3799/dqkx.2023.095

Citation:

Sun Xun, Liu Chaohui, Duan Ruihan, 2024. The Age and Geological Significance of Early Neoproterozoic Mafic Sills on the Eastern Margin of the North China Craton: Evidence from Zirconology. Earth Science, 49(9): 3122-3139. doi: 10.3799/dqkx.2023.095

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The Age and Geological Significance of Early Neoproterozoic Mafic Sills on the Eastern Margin of the North China Craton: Evidence from Zirconology

doi: 10.3799/dqkx.2023.095

Sun Xun^{1, 3
,
,},
Liu Chaohui^{1, 2
,
,
,},
Duan Ruihan⁴

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Civil and Resources Engineering, University of Science and Technology Beijing, Beijing 100083, China
3.
Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 511458, China
4.
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

Received Date: 2023-01-13
Available Online: 2024-10-16
Publish Date: 2024-09-25

Abstract

Abstract

The tectonic setting of the Neoproterozoic mafic sills (dykes) in the eastern margin of the North China Craton is of great significance for reconstructing the position of the Craton in Rodinia supercontinent. By analyzing the structure, paragenetic relationship with other minerals, and trace element characteristics of zircons in four mafic rock sill samples from Dalian and Xuzhou regions, it is found that they have typical structural and trace element characteristics of mafic magmatic zircons. Most of the crystallization temperatures (about 800-900 ℃) are consistent with those of zircons in mid-ocean ridge basalts, and some zircons can be observed to appear in clinopyroxene as inclusions. The above characteristics indicate that these zircons were formed in the early stage of cooling crystallization of mafic magma. Their U-Pb ages (881 Ma, 876 Ma, 914 Ma, and 925 Ma) can represent the emplacement age of mafic sills, and their trace elements show the characteristics of continental island arc magmatic zircons. Based on the geometric distribution of mafic sills (dykes) and the duration of magmatic activity, we suggest that they may have formed in a subduction related tensile environment.
- mafic sill,
- Neoproterozoic,
- North China Craton,
- zirconology,
- geochronology,
- mineralogy

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References(86)

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