1887

Abstract

Summary

East-Siberian and North Chuckchi seas shelfs was the area of intensive deltaic sedimentation during Aptian-Late Cretaceous and Cenozoic times. Large deltaic systems prograded at distance of hundreds kilometers building up continental terraces. Thick sedimentary infill related to two clastic pulses: Aptian-Late Cretaceous and Cenozoic. A number of a paleogeographic maps reflect the major sedimentary epochs.

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/content/papers/10.3997/2214-4609.201802441
2018-09-10
2024-04-26
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References

  1. GongC., SteelR.J.. WangY., LinC., OlariuC.
    [2016] Grain size and transport regime at shelf edge as fundamental controls on delivery of shelf-edge sands to deepwater. In: Earth-Science Reviews157, 32–60
    [Google Scholar]
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