An Alpine-style Ordovician collision complex in the Sierra de Pie de Palo, Argentina: Record of subduction of Cuyania beneath the Famatina arc
The Caucete Group and structurally overlying Pie de Palo Complex in western Argentina are characterised by two generations of west-verging folds and thrust-related shear zones, which formed under amphibolite facies conditions. The Caucete Group is separated from the Pie de Palo Complex by the Pirqui...
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| Autores principales: | Vujovich, Graciela Irene, Naipauer, Maximiliano |
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| Publicado: |
2011
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| Materias: | |
| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01918141_v33_n3_p343_vanStaal http://hdl.handle.net/20.500.12110/paper_01918141_v33_n3_p343_vanStaal |
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