Basal complex of Fuerteventura (Canary Islands) is an oceanic intrusive complex with rift-system affinities
- 1 October 1975
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 257 (5526), 469-471
- https://doi.org/10.1038/257469a0
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- Geochemical variation trends between the different Canary Islands in relation to their geological positionLithos, 1973
- Is the Betancuria Massif, Fuerteventura, Canary Islands, an Uplifted Piece of Oceanic Crust?Nature Physical Science, 1973
- Potassium-argon ages, volcanic stratigraphy, and geomagnetic polarity history of the Canary Islands; Lanzarote, Fuerteventura, Gran Canaria, and La GomeraAmerican Journal of Science, 1971
- The Troodos Massif, Cyprus and other ophiolites as oceanic crust: evaluation and implicationsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- East Canary Islands as a Microcontinent within the Africa–North America Continental Drift FitNature, 1970
- Is the Troodos Massif of Cyprus a Fragment of Mesozoic Ocean Floor?Nature, 1968
- Mesozoische Flysch-Ablagerungen auf der Kanareninsel FuerteventuraInternational Journal of Earth Sciences, 1968
- Contrasting Origins of the Eastern and Western Islands of the Canarian ArchipelagoNature, 1968
- Metamorphism in the Mid-Atlantic Ridge, 22°N latitudeMarine Geology, 1966