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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 the process of sea-floor
spreading. The methods and techniques used in paleomagnetic studies
of continental rocks and of the ocean floor are described and then
applied to determining horizontal movements of the Earth's crust
over geological time. An up-to-date review of global paleomagnetic
data enables 1000 million
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