Magnetic anomalies in the canary basin and the Mesozoic evolution of the central North Atlantic

• Published in: Marine Geophysical Researches
• Main Authors: Roest, W.R., Dañobeitia, Juan José, Verhoef, J., Collette, B. J.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Elsevier 1992
• Subjects: North Atlantic
• Online Access: http://hdl.handle.net/10261/201203; https://doi.org/10.1007/BF01674063

23 pages, 16 figures, 1 table The data from a recent magnetic compilation by Verhoef et al. (1991) off west Africa were used in combination with data in the western Atlantic to review the Mesozoic plate kinematic evolution of the central North Atlantic. The magnetic profile data were analyzed to identify the M-series sea floor spreading anomalies on the African plate. Oceanic fracture zones were identified from magnetic anomalies and seismic and gravity measurements. The identified sea floor spreading anomalies on the African plate were combined with those on the North American plate to calculate reconstruction poles for this part of the central Atlantic. The total separation poles derived in this paper describe a smooth curve, suggesting that the motion of the pole through time was continuous. Although the new sea floor spreading history differs only slightly from the one presented by Klitgord and Schouten (1986), it predicts smoother flowlines. On the other hand, the sea floor spreading history as depicted by the flowlines for the eastern central Atlantic deviates substantially from that of Sundvik and Larson (1988). A revised spreading history is also presented for the Cretaceous Magnetic Quiet Zone, where large changes in spreading direction occurred, that can not be resolved when fitting magnetic isochrons only, but which are evident from fracture zone traces and directions of sea floor spreading topography. © 1992 Kluwer Academic Publishers