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The sea floor: an introduction to marine geology [Libro electrónico] / autores: Eugen Seibold, Wolfgang H. Berger

Por: Seibold, Eugen [autor/a].
Berger, Wolfgang H [autor/a].
Tipo de material: Libro en línea Libro en línea Editor: New York, New York, United State: Springer-Verlag, c1993Edición: Segunda edición.Descripción: xiii, 356 páginas : ilustraciones ; 24 centímetros.ISBN: 3540568840; 0387568840; 9783662225219 (Print); 9783662225196 (Online).Tema(s): Submarine geologyNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 307-314 Número de sistema: 56589Contenidos:Mostrar Resumen:
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Man's understanding of how this planet is put together and how it evolved has changed radically during the last 30 years. This great revolution in geology - now usually subsumed under the concept of Plate Tectonics - brought the realization that convection within the Earth is responsible for the origin of today's ocean basins and conti­ nents, and that the grand features of the Earth's surface are the product of ongoing large-scale horizontal motions. Some of these notions were put forward earlier in this century (by A. Wegener, in 1912, and by A. Holmes, in 1929), but most of the new ideas were an outgrowth of the study of the ocean floor after World War II. In its impact on the earth sciences, the plate tectonics revolution is comparable to the upheaval wrought by the ideas of Charles Darwin (1809-1882), which started the intense discussion on the evolution of the biospere that has recently heated up again. Darwin drew his inspiration from observations on island life made during the voyage of the Beagle (1831-1836), and his work gave strong impetus to the first global oceanographic expedition, the voyage of HMS Challenger (1872- 1876). Ever since, oceanographic research has been intimately associ­ ated with fundamental advances in the knowledge of Earth. This should come as no surprise. After all, our planet's surface is mostly ocean.

Recurso en línea: http://link.springer.com/openurl?genre=book&isbn=978-3-662-22521-9
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Tipo de ítem Biblioteca actual Colección Signatura Estado Fecha de vencimiento Código de barras
Libros Biblioteca Electrónica
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Incluye bibliografía e índice: páginas 307-314

1. Introduction.. 2. Origin and morphology of ocean basins.. 3. Origin and morphology of ocean margins.. 4. Sources and composition of marine sediments.. 5. Effects of waves and currents.. 6. Sea level processes and effects of sea level change.. 7. Productivity and benthic organisms - distribution, activity, and environmental reconstruction.. 8. Imprint of climatic zonation on marine sediments.. 9. Deep-sea sediments - patterns, processes, and stratigraphic methods.. 10. Paleoceanography - the deep-sea record.. 11. Resources from the ocean floor.. 12. Epilog.. Subject Index

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Man's understanding of how this planet is put together and how it evolved has changed radically during the last 30 years. This great revolution in geology - now usually subsumed under the concept of Plate Tectonics - brought the realization that convection within the Earth is responsible for the origin of today's ocean basins and conti­ nents, and that the grand features of the Earth's surface are the product of ongoing large-scale horizontal motions. Some of these notions were put forward earlier in this century (by A. Wegener, in 1912, and by A. Holmes, in 1929), but most of the new ideas were an outgrowth of the study of the ocean floor after World War II. In its impact on the earth sciences, the plate tectonics revolution is comparable to the upheaval wrought by the ideas of Charles Darwin (1809-1882), which started the intense discussion on the evolution of the biospere that has recently heated up again. Darwin drew his inspiration from observations on island life made during the voyage of the Beagle (1831-1836), and his work gave strong impetus to the first global oceanographic expedition, the voyage of HMS Challenger (1872- 1876). Ever since, oceanographic research has been intimately associ­ ated with fundamental advances in the knowledge of Earth. This should come as no surprise. After all, our planet's surface is mostly ocean. eng

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