Palaeomagnetic study of Tertiary sedimentary rocks from Puna Salteña: Determination of clockwise rotations

On the Argentine Puna two phases of deformation, Late Tertiary and Quaternary, are recognized. Studies of Nazca-South American plate motions indicate convergence towards 77° ± 12° since 10 Ma. Although Tertiary shortening is not parallel to this direction, Quaternary shortening concides with it. Thi...

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Detalles Bibliográficos
Publicado: 1996
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v51_n3_p261_Prezzi
http://hdl.handle.net/20.500.12110/paper_00044822_v51_n3_p261_Prezzi
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