Sediments of MIS 5e age suggested by new OSL dates from the Skilvika section, west Svalbard
The sediment succession at Skilvika, west Svalbard, represents one of the key stratigraphic records of the Late Quaternary palaeoenvironments and glaciation history of the Svalbard/ Barents Sea area. A formation of raised marine sediments, interfingering with and capped by glacial deposits of local...
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Format: | Article in Journal/Newspaper |
Language: | English |
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Norwegian Polar Institute
2018
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Online Access: | https://polarresearch.net/index.php/polar/article/view/2659 |