Abstract
Neogene tectonic activity (Betic Orogeny) along the southern plate boundary of Iberia, as it converged with Africa and the Alboran Plate was inserted between them, propagated along Iberia's west side as far north as Galicia, northwest Spain. As the activity propagated northward, it reactivated structures formed during the Paleozoic (Hercynian), the Early Cretaceous opening of the northern North Atlantic and the Bay of Biscay, and the Paleogene Pyrenean Orogeny when Iberia collided with Eurasia. Recent earthquakes indicate that this tectonism is still active today as far north as northwest Spain.
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Acknowledgements
This study was funded by the Spanish Comision Interministerial de Ciencia y Tecnologia (CICYT) under project no. Mar-95-1953. We wish to express our appreciation to the Instituto Español de Oceanografia, Universidade de Vigo and Xunta de Galicia for their help during this investigation. Thanks also are extended to the captain and crew of the B/O Francisco de Paula Navarro for their cooperation during the cruise. The earthquake data for the region were compiled by S.T. Bolmer and W. Robertson V of Woods Hole Oceanographic Institution from the United States Geologic Survey National Earthquake Information Center, the World Data Center A for Seismology, and the Council of the National Seismic System (NCSS). R. Gómez and A. Martínez of the Instituto Español de Oceanografia, and D.L. Gray of Woods Hole Oceanographic Institution drafted the illustrations. We wish to thank J.A. Austin Jr. for his comments and suggestions during the preparation of this paper. Contribution no. 10936 of Woods Hole Oceanographic Institution.
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Muñoz, A., Acosta, J. & Uchupi, E. Cenozoic tectonics on the Galicia margin, northwest Spain. Geo-Mar Lett 23, 72–80 (2003). https://doi.org/10.1007/s00367-003-0126-1
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DOI: https://doi.org/10.1007/s00367-003-0126-1