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Different geophysical methods are used to study and map submarine permafrost on the Arctic Shelf. Due to specific features of submarine permafrost, none of geophysical methods can provide conclusive data when gas-charged sediments and taliks occur within permafrost. Experimental data show that electrical properties of frozen grounds change significantly.
№ | Имя | Описание | Имя файла | Размер | Добавлен |
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1. | Полный текст | poster.jpg | 21,8 МБ | 18 мая 2016 [gunar_91] |