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Sea-ice and iceberg sedimentation in the ocean: recent and past [Libro electrónico] / autor: Alexander P. Lisitzin

Por: Lisitsin, Alexander P [autor/a].
Tipo de material: Libro en línea Libro en línea Editor: New York, New York, United States: Springer, c2002Descripción: xi, 563 páginas : ilustraciones ; 28 centímetros.ISBN: 3540679650; 9783642632365 (Print); 9783642559051 (Online).Tema(s): Varves | Marine sediments | Submarine geologyNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 499-540 Número de sistema: 55894Contenidos:Mostrar Resumen:
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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.

Recurso en línea: http://link.springer.com/openurl?genre=book&isbn=978-3-642-63236-5
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Incluye bibliografía e índice: páginas 499-540

Chapter 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.. Index

Disponible para usuarios de ECOSUR con su clave de acceso

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. eng

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