1887

Abstract

Summary

Present article represents geologic and structural features of Late Quaternary paleo-valley network on the northernmost part of Barents-Kara shelf. Upper regional unconformity (URU) and erosion markers were plotted within the studied area.

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/content/papers/10.3997/2214-4609.202152135
2021-04-26
2024-06-15
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References

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