Sea-ice and iceberg sedimentation in the ocean : recent and past /
In many geological 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....
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| Format: | eBook |
| Language: | English |
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Berlin ; New York :
Springer,
[2002]
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| Online Access: | Connect to the full text of this electronic book |
Table of Contents:
- pt. I. The earth's cryosphere and peculiarities of sedimentation in it
- pt. II. Sea-ice sedimentation in the ocean
- pt. III. Glacial (iceberg) sedimentation in the ocean
- pt. IV. Glacial sedimentogenesis in the earth's geological past
- pt. V. Basis for the analysis of cryogenic formations : tectonic zonality.