On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic
It is possible to recognise four major Cenozoic regressive-transgresstve cycles along the coast of eastern Arctic Russia. Direct morphological and sedimentological evidence of old shorelines is abundant both as raised and submerged forms. Relic barrier and lagoon facies have been located on the shal...
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Journal of Coastal Research
1986
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ftfloridaojojs:oai:journals.flvc.org:article/77450 2023-05-15T14:50:43+02:00 On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic Puminov, A P. Degtyarenko, Y. P. 1986-06-13 application/pdf https://journals.flvc.org/jcr/article/view/77450 eng eng Journal of Coastal Research https://journals.flvc.org/jcr/article/view/77450/74930 https://journals.flvc.org/jcr/article/view/77450 Journal of Coastal Research; Vol 2 No 3 (1986): Journal of Coastal Research 0749-0208 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 1986 ftfloridaojojs 2020-11-14T19:08:43Z It is possible to recognise four major Cenozoic regressive-transgresstve cycles along the coast of eastern Arctic Russia. Direct morphological and sedimentological evidence of old shorelines is abundant both as raised and submerged forms. Relic barrier and lagoon facies have been located on the shallow shelf, forming complex on- and offlap facies assemblages. In places evidence has been disturbed by recent tectonic activity. Changes in sea-level are also reflected in aggradation-degradation stratigraphic sequences in coastal valleys and terraces. It is postulated that the most recent sea-level cycle is as yet unfinished, and will culminate in a transgression 2,000 yrs from now. Article in Journal/Newspaper Arctic Florida Online Journals (FloridaOJ) Arctic |
institution |
Open Polar |
collection |
Florida Online Journals (FloridaOJ) |
op_collection_id |
ftfloridaojojs |
language |
English |
description |
It is possible to recognise four major Cenozoic regressive-transgresstve cycles along the coast of eastern Arctic Russia. Direct morphological and sedimentological evidence of old shorelines is abundant both as raised and submerged forms. Relic barrier and lagoon facies have been located on the shallow shelf, forming complex on- and offlap facies assemblages. In places evidence has been disturbed by recent tectonic activity. Changes in sea-level are also reflected in aggradation-degradation stratigraphic sequences in coastal valleys and terraces. It is postulated that the most recent sea-level cycle is as yet unfinished, and will culminate in a transgression 2,000 yrs from now. |
format |
Article in Journal/Newspaper |
author |
Puminov, A P. Degtyarenko, Y. P. |
spellingShingle |
Puminov, A P. Degtyarenko, Y. P. On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic |
author_facet |
Puminov, A P. Degtyarenko, Y. P. |
author_sort |
Puminov, A P. |
title |
On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic |
title_short |
On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic |
title_full |
On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic |
title_fullStr |
On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic |
title_full_unstemmed |
On the Shoreline Dynamics of Russian East Arctic Seas During the Cenozoic |
title_sort |
on the shoreline dynamics of russian east arctic seas during the cenozoic |
publisher |
Journal of Coastal Research |
publishDate |
1986 |
url |
https://journals.flvc.org/jcr/article/view/77450 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Journal of Coastal Research; Vol 2 No 3 (1986): Journal of Coastal Research 0749-0208 |
op_relation |
https://journals.flvc.org/jcr/article/view/77450/74930 https://journals.flvc.org/jcr/article/view/77450 |
_version_ |
1766321762874687488 |