Génesis de ultramilonitas blancas en la falla de Azuaga (anticlinorio Badajoz-Córdoba)

[ES] Las ultramilonitas blancas de la falla de Azuaga se han formado por un metasomatismo silíceo-sódico y deformación dúctil a temperaturas bajas de blastomilonitas anteriores durante el funcionamiento sinextrorso de la falía. La composición química de las ultramilonitas blancas y blastomilonitas s. 1. asociadas parecen sugerir un origen ígneo.

[EN] White ultramylonites have been formed by Si-Na metasomatism and low temperature ductile deformation of blastomylonites resulting from the sinistral movement of the Azuaga fault. The major element composition of 14 samples of white ultramylonites and the associated blastomylonites suggests an igneous origin.

Peer reviewed

Country

Spain

Related Organizations

Spanish National Research Council
Spain

Keywords

Falla de Azuaga, Ultramilonitas blancas

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