Earth's oldest hotspot track at ca. 1.8 Ga advected by a global subduction system

Peng, Peng; Xu, Huiru; Mitchell, Ross N.; Teixeira, Wilson; Kirscher, Uwe; Qin, Zhaoyuan; Oliveira, Elson P.; Girardi, Vicente Antônio Vitório; Wang, Chong; Chemale, Farid

doi:10.1016/j.epsl.2022.117530

Cited by 20 publications

(11 citation statements)

References 48 publications

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“…1.77-1.75 Ga Yanggao-Fengzhen mafic dykes and ca. 1.74-1.73 Ga Miyun mafic dykes were sourced from enriched mantle and prevalent/high-μ mantle magma sources, respectively (e.g., Han et al, 2020;Peng, 2015;Peng et al, 2022;Wu, Wang, et al, 2022; this study).…”

Section: Detrital Zircon Ages and Isotope Concentrations From The Nor...mentioning

confidence: 90%

“…1.63 Ga Taishan large igneous provinces. Peng et al (2022) further proposed that the Xiong'er large igneous province represents the mantle plume center of the oldest hotspot track since ca. 1.8 Ga.…”

Section: Paleoproterozoic Tectonic Evolution Of the Northern North Ch...mentioning

confidence: 99%

“…Alternative to interpretations of modern-style plate tectonic events, researchers have proposed that vertical plume-related tectonics involving crustal delamination and volcanic resurfacing are evidenced in the Archean-Paleoproterozoic rock record. For example, Peng et al (2022) proposed that large igneous provinces across portions of the extinct Columbia-Nuna supercontinent reflect the occurrence of a ca. 1.8 Ga pulsating plume that was responsible for ancient plate motion.…”

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confidence: 99%

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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: Detrital Zircon Ages and Isotope Concentrations From The Nor...mentioning

confidence: 90%

Section: Paleoproterozoic Tectonic Evolution Of the Northern North Ch...mentioning

confidence: 99%

mentioning

confidence: 99%

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

Wang

Zuza

et al. 2022

Geochem Geophys Geosyst

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“…Megasequence 1 shows great similarity in detrital zircon age populations with the Xihe Group in the ENCC, especially the Svaerholt succession of the Kalak Nappe rocks (Kirkland et al, 2007(Kirkland et al, , 2008Zhang, Roberts, & Pease, 2016) This connection is quantitatively evaluated by our ENCC-NAUS model in the present study (Figure 3A). In fact, the NCC-NAUS connection in the Nuna supercontinent has been proved by paleomagnetic data (Kirscher et al, 2021;Pisarevsky et al, 2014;Wang et al, 2019;Zhang et al, 2012), detrital zircons (Yang et al, 2018(Yang et al, , 2019, oceanic euxinic events (Mitchell et al, 2021) and 1.8-1.6 Ga (Peng et al, 2022) and 1.3 Ga (Zhang et al, 2017) large igneous provinces. However, as indicated by paleomagnetic data, at ca.…”

Section: ~10 Ga Encc-naus Connectionmentioning

confidence: 91%

“…This connection is quantitatively evaluated by our ENCC–NAUS model in the present study (Figure 3A). In fact, the NCC–NAUS connection in the Nuna supercontinent has been proved by paleomagnetic data (Kirscher et al, 2021; Pisarevsky et al, 2014; Wang et al, 2019; Zhang et al, 2012), detrital zircons (Yang et al, 2018, 2019), oceanic euxinic events (Mitchell et al, 2021) and 1.8–1.6 Ga (Peng et al, 2022) and 1.3 Ga (Zhang et al, 2017) large igneous provinces. However, as indicated by paleomagnetic data, at ca.…”

Section: Introductionmentioning

confidence: 95%

Eastern North China Craton–North Australia Craton connection at 1.0 Ga through detrital zircon mixing modelling

Zhang

Liu

et al. 2022

Terra Nova

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In the ca. 1.0 Ga paleogeographic reconstruction, the North China Craton (NCC) is placed near Siberia, Laurentia, the Northern Australia Craton (NAUS), Baltica or India. To distinguish among these possibilities, we present inverse Monte Carlo modelling of the Xihe Group from the eastern NCC (ENCC), which is dominated by Grenvillian orogeny‐related detrital zircon age peaks, and of potential provenances (including NAUS, Siberia, Laurentia, India and the North Atlantic region). The result reveals that the ENCC–NAUS connection model yields the best mean cross‐correlation coefficient (R2 = ~0.92), which is also supported by the similarity in median εHf values between the Qiaotou Formation (Xihe Group) and the Jamison sandstones from the NAUS. The NCC–NAUS connection possibly records the breakup of Nuna and the assembly of Rodinia.

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A database of detrital zircon U–Pb ages in the North China Craton from the Paleoproterozoic to the early Palaeozoic

Dong,

Zuo,

Xiao

et al. 2023

Geoscience Data Journal

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U–Pb dating of detrital zircon is widely used in geology to identify the source of sediments and constrain palaeogeography and tectonic history. We collected the detrital zircon from the Paleoproterozoic to early Palaeozoic strata to understand the North China Craton's geological chronological characteristics. After screening and sorting out data information, we managed and analysed 84 papers from 2006 to 2022. Three hundred seventy‐nine samples comprising 29,431 pieces of U–Pb ages of detrital zircons gathered from the Proterozoic to Ordovician sedimentary rocks in North China Craton (NCC). Detrital zircons within five areas in the NCC, i. e., Xuhuai Basin, Zhaertai‐Bayan Obo‐Huade Basin, Yanliao Basin, Xiong'er Basin and Alxa Block, are discussed in detail. Meanwhile, we collected 2,588 pieces of Lu‐Hf detrital zircon data in the study. This Database can be helpful in understanding and explaining the tectonic evolution of the NCC from the Paleoproterozoic to the Early Palaeozoic.

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Earth's oldest hotspot track at ca. 1.8 Ga advected by a global subduction system

Cited by 20 publications

References 48 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

Eastern North China Craton–North Australia Craton connection at 1.0 Ga through detrital zircon mixing modelling

A database of detrital zircon U–Pb ages in the North China Craton from the Paleoproterozoic to the early Palaeozoic

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