Vol. XX, No. 1 (January–March 2016)

CONTENTS

REGIONAL PROBLEMS OF GEOCRYOLOGY

  • Pastukhov A.V., Marchenko-Vagapova T.I., Kaverin D.A., Goncharova N.N. Genesis and evolution of peat plateuas in the sporadic permafrost area in the European North-East (middle basin of the Kosyu river)
    | abstract

  • Veremeeva A.A., Glushkova N.V. Formation of relief in the regions of Ice Complex depositsdistribution: remote sensing and GIS studies in the Kolyma lowland tundra
    | abstract

ECOLOGICAL PROBLEMS OF EARTH’S CRYOLOGY

  • Dementyev M.S. Hydrobiological implications of and methods for determining dust pollution level of nival-glacial systems
    | abstract

PHYSICO-CHEMIKAL PROCESSES IN ICE AND FROZEN GROUND

  • Volokhov S.S. Mechanocalorical effect in frozen ground under uniaxial compression
    | abstract

CRYOGENIC PROCESSES AND FORMATIONS

  • Vasil’chuk Yu.K., Budantseva N.A., Vasil’chuk A.C., Podborny Ye.Ye., Chizhova Ju.N. Multistage Holocene massive ground ice in northern West Siberia
    | abstract

CRYOGENIC PROCESSES ON SHELF AND COAST OF ARCTIC SEAS

  • Pizhankova E.I. Modern climate change at high latitudes and its influence on the coastaldynamics of the Dmitriy Laptev Strait area
    | abstract

GAS HYDRATE FORMATION

  • Vasil’eva Z.A., Efimov S.I., Yakushev V.S. Prediction of thermal interaction betweenoil/gas wells and intra-permafrost metastable gas hydrates
    | abstract

RELIABILITY OF BASEMENTS AND STRUCTURES IN CRYOLITHOZONE

  • Zabolotnik S.I., Zabolotnik P.S. Ground temperature dynamics around and beneaththe Yakutsk Combined Heat and Power plant buildings
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METHODS OF PERMAFROST STUDIES

  • Kravtsova V.I., Rodionova T.V. Variations in size and number of thermokarst lakesin different permafrost regions: spaceborne evidence
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  • Popov S.V., Polyakov S.P. Ground-penetrating radar sounding of ice crevasses in the areaof the Russian Progress and Mirny stations (East Antarctica) during the field seasonof 2014/15
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  • Novikov E.A., Shkuratnik V.L., Oshkin R.O. Acoustic emission patterns as guides to unfrozen water in frozen soils
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