Compressional tectonic inversion of the Algero-Balearic basin: Latemost Miocene to present oblique convergence at the Palomares margin (Western Mediterranean)

Compressional tectonic inversion of the Algero-Balearic basin: Latemost Miocene to present oblique convergence at the Palomares margin (Western Mediterranean)

Interpretation of new multichannel seismic reflection profiles indicates that the Palomares margin was formed by crustal-scale extension and coeval magmatic accretion during middle to late Miocene opening of the Algero-Balearic basin. The margin formed at the transition between thinned continental c...

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Main Authors: Giaconia, Flavio (Author), Booth-Rea, Guillermo (Author), Ranero, César R. (Author), Gràcia, Eulàlia (Author), Bartolome, Rafael (Author), Calahorrano, Alcinoe (Author), Lo Iacono, Claudio (Author), Vendrell, Montserrat G. (Author), Cameselle, Alejandra L. (Author), Costa, Sergio (Author), Gómez de la Peña, Laura (Author), Martínez-Loriente, Sara (Author), Perea, Hector (Author), Viñas, Marina (Author)
Format: Article
Language:English
Published: 2015-07.
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