Iberian plate kinematics: A jumping plate boundary between Eurasia and Africa
Nature
By: S.P. Srivastava, Hans Schouten, W.R. Roest, Kim D. Klitgord, L.C. Kovacs, J. Verhoef, and R. Macnab
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Abstract
THE rotation of Iberia and its relation to the formation of the Pyrenees has been difficult to decipher because of the lack of detailed sea-floor spreading data, although several models have been proposed1-7. Here we use detailed aeromagnetic measurements from the sea floor offshore of the Grand Banks of Newfoundland to show that Iberia moved as part of the African plate from late Cretaceous to mid-Eocene time, with a plate boundary extending westward from the Bay of Biscay. When motion along this boundary ceased, a boundary linking extension in the King's Trough to compression along the Pyrenees came into existence. Finally, since the late Oligocene, Iberia has been part of the Eurasian plate, with the boundary between Eurasia and Africa situated along the Azores-Gibraltar fracture zone.
Suggested Citation
Srivastava, S., Schouten, H., Roest, W., Klitgord, K.D., Kovacs, L., Verhoef, J., and Macnab, R., 1990, Iberian plate kinematics: A jumping plate boundary between Eurasia and Africa: Nature, v. 344, no. 6268, p. 756-759, https://doi.org/10.1038/344756a0.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Iberian plate kinematics: A jumping plate boundary between Eurasia and Africa |
| Series title | Nature |
| DOI | 10.1038/344756a0 |
| Volume | 344 |
| Issue | 6268 |
| Year Published | 1990 |
| Language | English |
| Contributing office(s) | Woods Hole Coastal and Marine Science Center |
| Description | 4 p. |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Nature |
| First page | 756 |
| Last page | 759 |