Thermokarst and land–ocean interactions, Laptev sea region, Russia
Ice complexes (ICs) formed during the Late Pleistocene regression (marine isotope stages 5–3) on the drained Laptev Sea shelf and coastal lowlands. These sediments can be several dozen metres thick (up to 40–60 m). Over wide areas the lower boundary of the ICs is situated below current sea level. At...
Main Authors: | , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/1099-1530(200004/06)11:23.0.CO;2-L |