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- W4256384586 abstract "Three well-developed raised marine shorelines along Nordenskioldkysten have been studied and correlated with the shoreline displacement since the last deglaciation. The marine limit of 64 m in the area is of Late Weichselian age and has been dated to 10,900- I1,OOO years B.P. An intermediate level at 50 m is estimated to be 10,600-10,000 years old and demonstrates a sea level stagnation probably caused by a glacier readvance in eastern Svalbard during the Younger Dryas. A Holocene transgression culminating shortly after 6,000 years B.P. has been stratigraphically demonstrated, and it probably correlates with the Tapes transgression of Scandinavia. No pre-Late Weichselian marine levels are found, and the large rebound can be attributed only to a Late Weichselian glaciation." @default.
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- W4256384586 date "1987-01-06" @default.
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- W4256384586 title "The Late Weichselian and Holocene shoreline displacement on the west-central coast of Svalbard" @default.
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- W4256384586 doi "https://doi.org/10.3402/polar.v5i1.6866" @default.
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