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Border of the Continental Margin of the Central Arctic Uplifts in Amundsen Basin in Siberia

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Abstract

The seismic structure of the complex underlying the stratified sedimentary cover in the Amundsen Basin in Siberia indicates that the formation of a large-scale rift-related basin lying on a hyper-extended continental crust preceded the spreading process in the Eurasian Basin.

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REFERENCES

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Authors and Affiliations

  1. Gramberg All-Russian Scientific Research Institute for Geology and Mineral Resources of the Ocean, 190121, St. Petersburg, Russia

    V. A. Poselov,  V. V. Butsenko, V. D. Kaminsky & S. M. Zholondz

Authors
  1. V. A. Poselov
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  2. V. V. Butsenko
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  3. V. D. Kaminsky
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  4. S. M. Zholondz
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Corresponding author

Correspondence to V. A. Poselov.

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Translated by M. Hannibal

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Poselov, V.A., Butsenko, V.V., Kaminsky, V.D. et al. Border of the Continental Margin of the Central Arctic Uplifts in Amundsen Basin in Siberia. Dokl. Earth Sc. 493, 539–543 (2020). https://doi.org/10.1134/S1028334X20070156

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  • DOI: https://doi.org/10.1134/S1028334X20070156

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