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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...

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Detalles Bibliográficos
Autores principales: McElhinny, Michael W, McFadden, Phillip L, Dmowska, Renata, Holton, James R, Rossby, H Thomas
Lenguaje:eng
Publicado: Academic Press 1999
Materias:
Acceso en línea:http://cds.cern.ch/record/1990439