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The 1.33–1.30 Ga Yanliao large igneous province in the North China Craton: Implications for reconstruction of the Nuna (Columbia) supercontinent, and specifically with the North Australian Craton

TLDR
Li et al. as mentioned in this paper used secondary ion mass spectrometry (SIMS) baddeleyite dating to show that the diabase sills are distributed over a region that is >600 km long and >200 km wide, with areal extent > 1.2 × 10 5 ǫ
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This article is published in Earth and Planetary Science Letters.The article was published on 2017-05-01. It has received 110 citations till now. The article focuses on the topics: Craton & Laurentia.

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Extending full-plate tectonic models into deep time: Linking the Neoproterozoic and the Phanerozoic

TL;DR: For the first time, a continuous full-plate model spanning 1 Ga to the present day was presented in this paper, which includes a revised and improved model for the Neoproterozoic-Cambrian (1000-520 Ma) that connects with models of the Phanerozoic.
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Geochronological and geochemical insights into the tectonic evolution of the Paleoproterozoic Jiao-Liao-Ji Belt, Sino-Korean Craton

TL;DR: In this paper, the authors synthesize the geochronological, geochemical, and isotopic data on the Paleoproterozoic igneous rocks in the JLJB.
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Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China

TL;DR: In this paper, the formation mechanisms and tectonic settings of these rift basins as the targets of deep Earth are discussed, based on the restoration of global positions of the three cratons by pre-existing paleomagnetic data and plate reconstruction.
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The supercontinent cycle

TL;DR: The supercontinent cycle is interpreted as both an effect and a cause of mantle convection, emphasizing the importance of both top-down and bottom-up geodynamics, and the coupling between them.
References
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Journal ArticleDOI

Approximation of terrestrial lead isotope evolution by a two-stage model

TL;DR: In this paper, a two-stage model for terrestrial lead isotope evolution is proposed, which permits the age of the earth to be that of the meteorite system and also yields good model ages for samples of all ages.
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Magmatism at rift zones: The generation of volcanic continental margins and flood basalts

TL;DR: In this paper, the authors show that the production of magmatically active rifted margins and the effusion of flood basalts onto the adjacent continents can be explained by a simple model of rifting above a thermal anomaly in the underlying mantle.
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Did the breakout of laurentia turn gondwanaland inside-out?

TL;DR: Comparative geology suggests that the continents adjacent to northern, western, southern, and eastern Laurentia in the Late Proterozoic were Siberia, Australia-Antarctica, southern Africa, and Amazonia-Baltica, respectively.
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Large igneous provinces: crustal structure, dimensions, and external consequences

TL;DR: In this article, the authors compile all known in situ LIPs younger than 250 Ma and analyze dimensions, crustal structures, ages, and emplacement rates of representatives of the three major LIP categories: Ontong Java and Kerguelen-Broken Ridge oceanic plateaus, North Atlantic volcanic passive margins, and Deccan and Columbia River continental flood basalts Crustal thickness ranges from 20 to 40 km, and the lower crust is characterized by high (70-76 km s?1) compressional wave velocities.
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