Titlebook: Sea-Ice and Iceberg Sedimentation in the Ocean; Recent and Past Alexander P. Lisitzin Book 2002 Springer-Verlag Berlin Heidelberg 2002 Arct

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epochs, glacial sediments are widespread. This type of sedimentation results from the interaction between atmosphere, cryosphere, hydrosphere and biosphere under temperatures ranging from 0 to -80. Two types of glacial sediments exists: those from sea-ice and those from icebergs. Both types can be s

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Materials and Methods with the names of K.F. Rul’e, G.E. Shchurovskii, B.F. Shmidt, A.P. Pavlov, P.A. Kropotkin, and after the Revolution — with the names of S.V. Obruchev, I.P. Gerasimov, K.K. Markov, M.P. Grichuk, A.A. Velichko, and others. Not only continental glacial boundaries have been studied but also lithology o

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