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Sr, C and O isotope composition of marbles from the Sierra de Ancasti, Eastern Sierras Pampeanas, Argentina: age and constraints for the Neoproterozoic-Lower Paleozoic evolution of the proto-Gondwana margin

The Sierra Brava Complex on the eastern flank of the Sierra de Ancasti consists of marbles, metabasites, calc-silicate rocks, psammo-pelitic schists and gneisses. In the central part of this sierra a thick succession of banded schists (Ancasti Formation) crops out. Regional metamorphism of these roc...

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Publicado en:Geologica Acta: an international earth science journal
Autores principales: J.A. Murra, E.G. Baldo, C. Galindo, C. Casquet, R.J. Pankhurst, C.W. Rapela, J. Dahlquist
Formato: Artigo
Lenguaje:Inglês
Publicado: Universitat de Barcelona 2011
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Acceso en línea:https://www.redalyc.org/articulo.oa?id=50522124008
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