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...
Main Authors: | , , , , , |
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Format: | Conference Object |
Language: | unknown |
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Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research International Permafrost Association
2016
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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 |