Shear zones as a result of intraplate tectonics in oceanic crust: the example of the Basal complex of fuerteventura (Canary Islands)

Author:

Fernandez Carlos,Casillas Ramon,Ahijado Agustina,Perello Virginia,Hernandez-Pacheco Alfredo

Publisher

Elsevier BV

Subject

Geology

Reference72 articles.

1. Potassiumargon ages, volcanic stratigraphy, and geomagnetic polarity history of the Canary Islands: Lanzarote, Fuerteventura, Gran Canada and La Gomera;Abdel-Monem;American Journal of Science,1971

2. Deformation styles adjacent to transform faults: evidence from the Troodos ophiolite, Cyprus;Allerton,1992

3. Volcanic evolution of the Fuerteventura Island in the light of new K-Ar data;Ancochea;Journal of Volcanology and Geothermal Research,1990

4. La Serie I de la isla de Fuerteventura;Ancochea;Memorias de la Real Academia de Ciencas Exactes, Física y Naturales de Madrid,1993

5. Constructive and destructive episodes in the building of a young oceanic island, La Palma, Canary Islands and genesis of the Caldera de Taburiente;Ancochea;Journal of Volcanology and Geothermal Research,1994

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