Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology

Liu, Xiaoguang; Zhang, Jian; Li, Sanzhong; Li, Xiyao; Yin, Changqing

doi:10.1007/s00531-019-01784-w

Cited by 7 publications

(2 citation statements)

References 47 publications

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“…2.05 Ga, and ca. 1.83 Ga (e.g., Cai et al., 2017; Chen et al., 2015; Cui et al., 2015; Diwu et al., 2008, 2010, 2013; Du et al., 2011, 2012, 2016, 2017; Duan et al., 2014, 2018; Gao & Santosh, 2019; Geng et al., 2012; Hu et al., 2012; C. Lan et al., 2017; Z. Lan et al., 2014; H. Li et al., 2013; M. Li et al., 2013; Q. Li et al., 2011; Q. Li, Liu,Wang, Chu, et al., 2008; Q. Li, Liu, Wang, Zhang, et al., 2008; X. Y. Li et al., 2020; C. H. Liu et al., 2014; C. H. Liu, Zhao, Liu, et al., 2012; C. H. Liu, Zhao, Sun, Wu, et al., 2011; C. H. Liu, Zhao, Sun, Zhang et al., 2011; C. H. Liu, Zhao, Sun, Zhang, & Yin, 2012; C. H. Liu, Zhao, Sun, Zhang, Yin, & He, 2012; C. H. Liu, Liu, et al., 2016; C. H. Liu, Zhao, et al., 2016; J. H. Liu et al., 2020; X. Liu et al., 2020; Lyu et al., 2019; M. Z. Ma et al., 2012; X. Ma et al., 2014; X. Ma, Fan, et al., 2013; X. Ma, Guo, et al., 2013; J. Meng et al., 2018; Y. Meng et al., 2018; Peng et al., 2017; L. Ren et al., 2013; R. Ren et al., 2011; Santosh et al., 2015; Shi et al., 2018; Sun et al., 2017, 2020; Tang et al., 2016; Y. S. Wan et al., 2006, 2010, 2011, 2012, 2015; F. Wang et al., 2011; J. Wang et al., 2010; J. P. Wang et al., …”

Section: Discussionmentioning

confidence: 99%

Paleoproterozoic Plate Tectonics Recorded in the Northern Margin Orogen, North China Craton

Wang

Zuza

et al. 2022

Geochem Geophys Geosyst

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Section: Discussionmentioning

confidence: 99%

Paleoproterozoic Plate Tectonics Recorded in the Northern Margin Orogen, North China Craton

Wang

Zuza

et al. 2022

Geochem Geophys Geosyst

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“…The spatial and vertical stratigraphic framework for the Huoshan Formation in the study area X. G. Liu et al, 2018), the Yan-Liao Rift in the northern and central NCC (X. G. Liu, Zhang, Li, Li, & Yin, 2020;Wen, 1989), and the Xiong'er Rift in the southern NCC (X. M.…”

Section: Geological Settingmentioning

confidence: 99%

Geochronological constraints of the Huoshan Formation in the Lüliang area: Implication on the Great Unconformity in the central North China Craton

2021

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The Great Unconformity between the Precambrian basement and the Phanerozoic successions marks a major gap in the stratigraphic records globally. However, previous studies on the time, magnitude, and the spatial distribution of this unconformity in the North China Craton (NCC) mainly focused on the south‐eastern margin and were seldom investigated in the central area. In this study, we report detrital zircon geochronological data of the Huoshan Formation, a siliciclastic stratigraphic unit between the Archean‐Palaeoproterozoic metamorphic basement and Cambrian successions in the central NCC. The youngest age peak of 685 Ma suggests that the Huoshan Formation was formed in the post‐Ediacaran rather than the counterpart of the lower Palaeo‐Mesoproterozoic Changcheng Group. The detrital zircons of the quartz sandstone from the Huoshan Formation show varied age populations of 2,700–2,600 Ma, 2,600–2,500 Ma, 2,200–2,000 Ma, 1,900–1,800 Ma, and 700–600 Ma, which correspond to typical tectono‐thermal events of the NCC. First, the widely developed Precambrian tectono‐thermal events in the NCC were archived in the detrital zircons in the Huoshan Formation, for instance, the crustal growth event at 2,600–2,500 Ma and the 1,850–1,800 Ma magmatic and metamorphic events. Second, the age peaks younger than 1,000 Ma are not distinct in the NCC and are possibly from other terranes. The Great Unconformity represented by the boundary between the Huoshan Formation and the underlying Archean‐Palaeoproterozoic basement suggested a high topography and long‐term denudation in the Lüliang area during the transition from the Proterozoic to the Phanerozoic.

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Detrital zircon U-Pb-Hf isotopes from the Yanliao intracontinental rift sediments: Implications for multiple phases of Neoarchean-Paleoproterozoic juvenile crustal growth in the North China Craton

Liu

Gao

et al. 2021

Gondwana Research

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Tectono-sedimentary evolution of the Mesoproterozoic basins in the southern Yan-Liao and Mianchi-Queshan areas: insights from stratigraphic pattern and detrital zircon geochronology

Cited by 7 publications

References 47 publications

Paleoproterozoic Plate Tectonics Recorded in the Northern Margin Orogen, North China Craton

Paleoproterozoic Plate Tectonics Recorded in the Northern Margin Orogen, North China Craton

Geochronological constraints of the Huoshan Formation in the Lüliang area: Implication on the Great Unconformity in the central North China Craton

Detrital zircon U-Pb-Hf isotopes from the Yanliao intracontinental rift sediments: Implications for multiple phases of Neoarchean-Paleoproterozoic juvenile crustal growth in the North China Craton

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