Magnetic evidence for slow seafloor spreading during the formation of the Newfoundland and Iberian margins

There is considerable debate concerning the nature and origin of the thin crust within the ocean–continent transition (OCT) zones of many passive non-volcanic continental margins, located between thinned continental and true oceanic crust. This crust is usually found to be underlain by upper mantle...

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Veröffentlicht in:	Earth and planetary science letters 2000-10, Vol.182 (1), p.61-76
Hauptverfasser:	Srivastava, S.P., Sibuet, J.-C., Cande, S., Roest, W.R., Reid, I.D.
Format:	Artikel
Sprache:	eng
Schlagworte:	continental margin magnetic anomalies Marine Newfoundland sea-floor spreading transition zones
Online-Zugang:	Volltext
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