Ice-wedge stable isotopes at the Dmitry Laptev Strait (Northeast Siberian Arctic) – indications for Late Quaternary stratigraphy and paleoclimate

Ice wedges are the most abundant type of ground ice in the ice-rich permafrost deposits of the Northeast Siberian Arctic. They are formed by the periodic repetition of frost cracking and subsequent crack filling and refreezing in spring, mostly by melt water of winter snow. Ice wedges can be studied...

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Bibliographic Details
Main Authors: Opel, Thomas, Wetterich, Sebastian, Dereviagin, Alexander Yu, Meyer, Hanno, Fuchs, Margret, Schirrmeister, Lutz
Format: Conference Object
Language:unknown
Published: Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research International Permafrost Association 2016
Subjects:
Yar
Ice
Online Access:https://epic.awi.de/id/eprint/42020/
https://epic.awi.de/id/eprint/42020/1/Poster_Oyogos_Opel_ICOP.pdf
https://hdl.handle.net/10013/epic.48815
https://hdl.handle.net/10013/epic.48815.d001