The scientists who first comprehensively studied magnetic striping in oceanic crust were Frederick Vine and Drummond Matthews. In 1963, they proposed the Vine-Matthews hypothesis, which linked the patterns of magnetic anomalies on the ocean floor to seafloor spreading and tectonic activity. Their work provided crucial evidence for the theory of plate tectonics, helping to explain how new oceanic crust is formed at mid-ocean ridges. Their findings were foundational in advancing our understanding of Earth's geological processes.
Copyright © 2026 eLLeNow.com All Rights Reserved.