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Paleomagnetism, 73: Continents and Oceans

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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 ...

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Paleomagnetism, 73: Continents and Oceans
1999, Academic Press, San Diego, CA

ISBN-13: 9780124833555

2nd Revised edition

Hardcover

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