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: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
2002
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Schlagworte: | |
Online-Zugang: | BTU01 Volltext |
Zusammenfassung: | 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. Both types can be subdivided into various subfacies. Most widespread in the Northern Hemisphere is the Siberian subfacies, characterized by silt and clay and often misinterpreted as sediments of temperate zones. This reference book for researchers working on this kind of sediments provides a complete overview of the various glacial deposits in the ocean |
Beschreibung: | 1 Online-Ressource (XI, 563 p) |
ISBN: | 9783642559051 |
DOI: | 10.1007/978-3-642-55905-1 |
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indexdate | 2024-07-10T08:10:48Z |
institution | BVB |
isbn | 9783642559051 |
language | English |
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physical | 1 Online-Ressource (XI, 563 p) |
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publishDate | 2002 |
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spelling | Lisitzin, Alexander P. Verfasser aut Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past by Alexander P. Lisitzin Berlin, Heidelberg Springer Berlin Heidelberg 2002 1 Online-Ressource (XI, 563 p) txt rdacontent c rdamedia cr rdacarrier 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. Both types can be subdivided into various subfacies. Most widespread in the Northern Hemisphere is the Siberian subfacies, characterized by silt and clay and often misinterpreted as sediments of temperate zones. This reference book for researchers working on this kind of sediments provides a complete overview of the various glacial deposits in the ocean Geography Geomorphology Oceanography Sedimentology Geology Erscheint auch als Druck-Ausgabe 9783642632365 https://doi.org/10.1007/978-3-642-55905-1 Verlag URL des Erstveröffentlichers Volltext |
spellingShingle | Lisitzin, Alexander P. Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past Geography Geomorphology Oceanography Sedimentology Geology |
title | Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past |
title_auth | Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past |
title_exact_search | Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past |
title_full | Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past by Alexander P. Lisitzin |
title_fullStr | Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past by Alexander P. Lisitzin |
title_full_unstemmed | Sea-Ice and Iceberg Sedimentation in the Ocean Recent and Past by Alexander P. Lisitzin |
title_short | Sea-Ice and Iceberg Sedimentation in the Ocean |
title_sort | sea ice and iceberg sedimentation in the ocean recent and past |
title_sub | Recent and Past |
topic | Geography Geomorphology Oceanography Sedimentology Geology |
topic_facet | Geography Geomorphology Oceanography Sedimentology Geology |
url | https://doi.org/10.1007/978-3-642-55905-1 |
work_keys_str_mv | AT lisitzinalexanderp seaiceandicebergsedimentationintheoceanrecentandpast |