Rotation of crustal domains related to Gondwanide deformation in the Neoproterozoic–Cambrian Sauce Chico Complex (Argentina), southwestern margin of the Río de la Plata Craton: Insights from AMS data

Author:

Vazquez Lucero S.E.,Ballivián Justiniano C.A.,Fazzito S.,Prezzi C.B.,Ruíz González V.,Rodríguez S.,Vizán H.

Publisher

Elsevier BV

Reference108 articles.

1. Provenance, volcanic record, and tectonic setting of the paleozoic Ventania Fold Belt and the Claromecó Foreland Basin: implications on sedimentation and volcanism along the southwestern Gondwana margin;Alessandretti;Journal of South American Earth Sciences,2013

2. Cuenca paleozoica de Ventania, sierras australes, provincia de Buenos Aires;Andreis,1989

3. Sedimentología y estratigrafía del grupo la Providencia (nom. nov.): cubierta superior neoproterozoica, sistema de tandilia, Argentina;Arrouy;Latin American Journal of Sedimentology and Basin Analysis,2015

4. Arzadún, G., Cisternas, M.E., Cesaretti, N.N., Tomezzoli, R.N. 2016a., Análisis de materia orgánica en niveles de carbón de la Formación Tunas (Pérmico de Gondwana), Cuenca de Claromecó, Provincia de Buenos Aires, Argentina. Revista de la Asociación Geológica Argentina., 73(4), 538–551.

5. Arzadún, G., Tomezzoli, R.N., Fortunatti, N., Cesaretti, N.N., Febbo, M.B., Calvagno, J.M., 2021. Deformation understanding in the Upper Paleozoic of Ventana Ranges at Southwest Gondwana Boundary. Scientific Reports, 11, 1–17. Nature Publishing Group UK.

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