Frederick J. Vine
Quick Summary
Frederick J. Vine was a British geophysicist who, along with Drummond H. Matthews, proposed a significant hypothesis in 1963 regarding marine magnetic anomalies. This hypothesis suggested that new oceanic crust, formed at mid-ocean ridges, records the Earth's magnetic field at the time of its formation.12
The theory posits that as magma wells up and cools at these spreading centers, it becomes magnetized. If the Earth's magnetic field is in a normal polarity, the crust shows a positive magnetic anomaly, and if it's in a reversed polarity, it shows a negative anomaly. These magnetized blocks, as they move away from the ridge, create a symmetrical pattern of magnetic bands on either side of the ridge axis, resembling a zebra's stripes. This groundbreaking idea played a crucial role in the development of the theory of plate tectonics.134
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