Magnetic Anomalies Over Oceanic Ridges¶
Vine, F. J., & Matthews, D. H. (1963). Magnetic Anomalies Over Oceanic Ridges.
Cited by¶
2 citations across 2 artifacts.
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Domain-specific¶
- Continental Drift
- Divergence Zone
- Fred Vine and Drummond Matthews (1963), independently of Lawrence Morley, showed that this replacement leaves a record: as new crust forms and cools through reversals of Earth's magnetic field, it locks in symmetric magnetic "stripes" mirrored on either side of the ridge axis, direct evidence that crust is continuously created at the divergence and spreads outward
This sourceProposes that new crust magnetised during successive geomagnetic reversals records seafloor spreading as ridge-parallel magnetic anomalies.
- Fred Vine and Drummond Matthews (1963), independently of Lawrence Morley, showed that this replacement leaves a record: as new crust forms and cools through reversals of Earth's magnetic field, it locks in symmetric magnetic "stripes" mirrored on either side of the ridge axis, direct evidence that crust is continuously created at the divergence and spreads outward
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