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Concerning tectonics and the tectonic evolution of the Arctic

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TLDR
Zonenshain et al. as mentioned in this paper demonstrated new geological data for the key structures of the Arctic, which are analyzed with consideration of new geophysical data (gravitational and magnetic), including first seismic tomography models for the Arctic.
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This article is published in Russian Geology and Geophysics.The article was published on 2013-08-01. It has received 84 citations till now. The article focuses on the topics: Arctic & 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.

The Timanide, Caledonide and Uralide orogens in the Eurasian high Arctic, and relationships to the p...

TL;DR: The Timanide, Caledonide and Uralide orogens in the Eurasian high Arctic and their relationships to the p... as discussed by the authors have been studied in the literature.
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Mesozoic–Cenozoic volcanism and geodynamic events in the Central and Eastern Arctic

TL;DR: In this paper, the patterns and history of Mesozoic-Cenozoic plume magmatism in the Arctic is considered in relation with suprasubduction volcanism and geodynamic events.
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Fold belts and sedimentary basins of the Eurasian Arctic

TL;DR: A review of the current state-of-the-art knowledge of Eurasian Arctic tectonics can be found in this paper, which highlights questions that remain to be addressed.
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Arctida between Rodinia and Pangea

TL;DR: In this paper, a new outlook on the history of Arctida was proposed, a continental mass that combined sialic blocks of the current Eurasian shelf of the Arctic Ocean.
References
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Tectonic models for accretion of the Central Asian Orogenic Belt

TL;DR: The Central Asian Orogenic Belt ( c. 1000-250 Ma) formed by accretion of island arcs, ophiolites, oceanic islands, seamounts, accretionary wedges, and oceanic plateaux and microcontinents in a manner comparable with that of circum-Pacific Mesozoic-Cenozoic orogens is studied in this article.
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Continental break-up and collision in the Neoproterozoic and Palaeozoic — A tale of Baltica and Laurentia

TL;DR: In this paper, it was shown that Laurentia and Baltica shared a common drift history for the time interval 750-600 Ma as they rotated clockwise and drifted southward from an equatorial position during the opening of the Proto-Pacific between Laurentia, and the two continents of Baltica and Laurentia witnessed the break-up of one supercontinent, Rodinia and the formation of another, but less long-lived, Pangea.
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Earth geography from 500 to 400 million years ago: a faunal and palaeomagnetic review

TL;DR: In this paper, a combination of palaeomagnetic and faunal data is used to reconstruct the changing palaeolatitudes of Baltica, Laurentia and Siberia.
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The Altaids of Central Asia: A tectonic and evolutionary innovative review

TL;DR: A review of the current understanding of the many inherent tectonic problems of the Altaids can be found in this paper, which is timely and appropriate to present a review of current understanding.
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