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Геохимический состав повторно-жильных льдов в Батагайской едоме
Васильчук Ю.К., Васильчук Д.Ю., Буданцева Н.А., Васильчук А.К., Гинзбург А.П.
The subject of this research is the syngenetic ice wedges stripped in the Batagaika crater (67
Ice Complex permafrost of MIS5 age in the Dmitry Laptev Strait coastal region (East Siberian Arctic)
Wetterich S., Tumskoy V., Rudaya N., Kuznetsov V., Maksimov F., Opel T., Meyer H., Andreev A., Schirrmeister L.
-like reticulated segregation ice. Two peaty horizons within the Buchchagy Ice Complex and syngenetic ice wedges (2
Ice Complex permafrost of MIS5 age in the Dmitry Laptev Strait coastal region (East Siberian Arctic)
Wetterich S., Tumskoy V., Rudaya N., Kuznetsov V., Maksimov F., Opel T., Meyer H., Andreev A., Schirrmeister L.
-like reticulated segregation ice. Two peaty horizons within the Buchchagy Ice Complex and syngenetic ice wedges (2
Ice Complex formation on Bol'shoy Lyakhovsky Island (New Siberian Archipelago, East Siberian Arctic) since about 200 ka
Wetterich S., Rudaya N., Kuznetsov V., Maksimov F., Opel T., Meyer H., Günther F., Bobrov A., Raschke E., Zimmermann H., Strauss J., Starikova A., Fuchs M., Schirrmeister L.
landscapes of unglaciated Beringia were largely shaped by ice-wedge polygon tundra. Ice Complex (IC) strata
Holocene thermokarst and pingo development in the Kolyma Lowland (NE Siberia)
Wetterich S., Schirrmeister L., Nazarova L., Palagushkina O., Bobrov A., Pogosyan L., Savelieva L., Syrykh L., Matthes H., Fritz M., Günther F., Opel T., Meyer H.
cracks by surface water with quasi-meteoric signature. Currently inactive syngenetic ice wedges formed
Late Quaternary paleoenvironmental records from the Chatanika River valley near Fairbanks (Alaska)
Schirrmeister L., Meyer H., Andreev A., Wetterich S., Kienast F., Bobrov A., Fuchs M., Sierralta M., Herzschuh U.
-like silt, and sand layers, penetrated by small ice wedges. OSL dates support a stadial early Wisconsin (MIS
Late Quaternary paleoenvironmental records from the Chatanika River valley near Fairbanks (Alaska)
Schirrmeister L., Meyer H., Andreev A., Wetterich S., Kienast F., Bobrov A., Fuchs M., Sierralta M., Herzschuh U.
-like silt, and sand layers, penetrated by small ice wedges. OSL dates support a stadial early Wisconsin (MIS
РАДИОВОЛНОВАЯ ДИАГНОСТИКА ЛЬДИСТЫХ ПОРОД В ЗОНЕ ТЕРМОКАРСТОВОГО ПРОВАЛА (П. БАТАГАЙ, ЯКУТИЯ)
Мельчинов В.П., Павлов А.А., Кладкин В.П., Башкуев Ю.Б., Хаптанов В. Б.
. It is established the spatial dependence of the thickness of frozen sediments with ice wedges by solving the inverse
Frozen barrier evolution in saturated porous media
Sheshukov A., Egorov A.
the condition for the special case when liquid water and ice can reside in the pore space simultaneously
Frozen barrier evolution in saturated porous media
Sheshukov A., Egorov A.
the condition for the special case when liquid water and ice can reside in the pore space simultaneously

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