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The cataclastic rocks autcrops are located at the northwestern Pampean Ranges and have a N-S direction. They are limiting the Famatina system to the eastern and carne along the Puna.  They have been recognized protomylonites, mylonite gneiss and mylonite schists which may be formed under 10 or 15 km of deep and 275-350&#194;&#176; C temperatures of source.  The main dominant structure have NNW direction and dips to the eastern. There can be seen compressive movements related to western blocks displacements.  During de Ocloyica distrophic phase (Upper Ordovician-Lower Silurian) may be formed these cataclastic rocks, related to the Antofalla Craton collision.  En las Sierras Pampeanas Noroccidentales del noroeste argentino se desarrolla una faja catacl&#225;stica de rumbo submeridional, en rocas del basamento &#237;gneo-metam&#243;rfico pertenecientes al Paleozoico Inferior. Esta estructura coincide con el l&#237;mite oriental del Sistema de Famatina y su porci&#243;n septentrional se extiende dentro de la provincia morfoestructural de la Puna.  En el &#225;rea estudiada se reconocen protomilonitas, gneises y esquistos milon&#237;ticos, los que, en base a sus caracter&#237;sticas texturales, se habr&#237;an formado a profundidades de 10 a 15 km y a temperaturas de 275-350&#194;&#176; C.  El plano principal de cizalla tiene rumbo NNW e inclina hacia el este y sobre el mismo se distinguen movimientos compresivos con desplazamientos relativos de bloques hacia el oeste.  La faja de cataclasitas se habr&#237;a originado durante la Fase Diastr&#243;fica Ocl&#243;yica (Ordov&#237;cico Superior-Sil&#250;rico Inferior) relacionada con la colisi&#243;n del Crat&#243;n de Antofalla

La faja cataclástica del borde oriental del Sistema de FamatIna, ArgentIna