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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弯曲道理

Mechanisms of Sediment Incorporation in Continental Ice-Catchment Areashree main approaches exist to solve this problem: (1) direct observations of the glacier activity (glaciohydrological investigations); (2) theoretic conclusions based on the laboratory experiments and models; (3) geomorphological investigations of both landforms appeared due to erosional activity of

睨视

Recent Iceberg-Rafted and Cryophilic Biogenic Deposits of Antarcticaarctic are icebergs spread over the area of 60-65 million km., i.e. the area is 5 times as great as the Arctic Ocean (Table 10.1). The second large area of iceberg-rafted deposits is situated in the Northern Hemisphere (Davis Strait, western and eastern coasts of Greenland, regions stretching southw

美丽的写

membrane

Cryogenic Faciesatures of bottom sediments related to it (including petrographic, mineralogic, structural-textural peculiarities and those related to biogenic component and initial stages of diagenesis, etc.). According to G. F. Krasheninnikov (1971), facies are considered as a sedimentary complex which differs fro

栖息地

打算

Sedimentary System of the Far Eastern Seas and North Pacificov Islands — along 57–58° N parallel — Komandorskie Islands — along Kamchatka coasts to its southernmost point. Warm waters entering the central parts of the sea via the straits between the Aleutian Islands shift the ice boundary to the north.

Melanocytes

Mechanisms of Sediment Incorporation in Continental Ice-Catchment Areasonclusions based on the laboratory experiments and models; (3) geomorphological investigations of both landforms appeared due to erosional activity of glaciers (fjords, troughs and other erosional forms) and accumulative landforms (different types of moraines, etc.).

HAIRY

exclusice

Lithology and Geochemistry of the Zones of Iceberg Sedimentationnvironmental conditions of their accumulation and their further evolution. Study of the modern processes allows solving this problem not on the basis of controversial guess-works but on the basis of comparative-lithologic method and understanding of real processes and their geologic consequences.