Texture and structure of the Late Holocene ground ice in the Northern West Siberia
The Late Holocene ground ices are occurred due to freeze cracking, slope, thermocast, thermoerosion pro‑ cesses. New formation ice within may intervene to the Pleistocene, lower Holocene ground ice and perma‑ frost and can really complicate their structure. Relationship between seasonal and perennia...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | Russian |
| Published: |
Nauka
2017-12-01
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| Series: | Lëd i Sneg |
| Subjects: | |
| Online Access: | https://ice-snow.igras.ru/jour/article/view/421 |