Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico
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.
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New York, New York, United States Springer
c200
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Subjects: | Varves, Marine sediments, Submarine geology, |
Online Access: | http://link.springer.com/openurl?genre=book&isbn=978-3-642-63236-5 |
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KOHA-OAI-ECOSUR:558942021-01-11T22:00:21ZSea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico Lisitsin, Alexander P. autor/a textNew York, New York, United States Springerc2002engIn 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.Incluye bibliografía e índice: páginas 499-540Chapter 1. Introduction.. Chapter 2. The earth's cryosphere and peculiarities of sedimentation in it.. Chapter 3. Sea ice sedimentation in the ocean.. Chapter 4. Glacial (iceberg sedimentation in the ocean.. Chapter 5. Glacial sedimentogenesis in the earth's geological past.. Chapter 6. Basis for the analysis of cryogenic formations • tectonic zonality.. IndexIn 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.Disponible en formato PDFSubscripción a ELSEVIERVarvesMarine sedimentsSubmarine geologyDisponible en líneahttp://link.springer.com/openurl?genre=book&isbn=978-3-642-63236-5URN:ISBN:3540679650URN:ISBN:9783642632365 (Print)URN:ISBN:9783642559051 (Online)Disponible para usuarios de ECOSUR con su clave de acceso |
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Varves Marine sediments Submarine geology Varves Marine sediments Submarine geology |
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Varves Marine sediments Submarine geology Varves Marine sediments Submarine geology Lisitsin, Alexander P. autor/a Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico |
description |
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. |
format |
Texto |
topic_facet |
Varves Marine sediments Submarine geology |
author |
Lisitsin, Alexander P. autor/a |
author_facet |
Lisitsin, Alexander P. autor/a |
author_sort |
Lisitsin, Alexander P. autor/a |
title |
Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico |
title_short |
Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico |
title_full |
Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico |
title_fullStr |
Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico |
title_full_unstemmed |
Sea-ice and iceberg sedimentation in the ocean recent and past Libro electrónico |
title_sort |
sea-ice and iceberg sedimentation in the ocean recent and past libro electrónico |
publisher |
New York, New York, United States Springer |
publishDate |
c200 |
url |
http://link.springer.com/openurl?genre=book&isbn=978-3-642-63236-5 |
work_keys_str_mv |
AT lisitsinalexanderpautora seaiceandicebergsedimentationintheoceanrecentandpastlibroelectronico |
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1756228022900359168 |