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Erschienen in:
2002 | OriginalPaper | Buchkapitel
Cryogenic Facies
verfasst von : Prof. Alexander P. Lisitzin
Erschienen in: Sea-Ice and Iceberg Sedimentation in the Ocean
Verlag: Springer Berlin Heidelberg
Enthalten in: Professional Book Archive
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In accordance with the most common definition of “facies” the author considers them to represent an unity of sedimentation environment and specific features 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 from neighbouring deposits of the same stratigraphical level.