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Paleomagnetism: continents and oceans
Paleomagnetism is the study of the fossil magnetism in rocks. It has been paramount in determining that the continents have drifted over the surface of the Earth throughout geological time. The fossil magnetism preserved in the ocean floor has demonstrated how continental drift takes place through t...
Autores principales: | McElhinny, Michael W, McFadden, Phillip L, Dmowska, Renata, Holton, James R, Rossby, H Thomas |
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Lenguaje: | eng |
Publicado: |
Academic Press
1999
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Materias: | |
Acceso en línea: | http://cds.cern.ch/record/1990439 |
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