C-O isotopes of the Ediacarian Loma Negra Formation in Barker area, Tandilia System, Argentina: diagenetic implications
C-O isotopes of the Ediacarian Loma Negra Formation in Barker area, Tandilia System, Argentina: diagenetic implications
The Neoproterozoic sedimentary succession of the Tandilia Basin is exposed in Olavarría and Barker areas and composed of the Villa Mónica, Cerro Largo, Las Aguilas, Olavarría and Loma Negra formations (Sierras Bayas Group) and the Cerro Negro Formation. On top of the Loma Negra Formation a regional unconformity, Barker Surface, was related to an important sea level fall which could be linked to Gaskiers glaciation, however no negative C isotopes excursions were observed.
Fil: Poire, Daniel Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Arrouy, Maria Julia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Gómez Peral, Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Canalicchio, José. Cementos Avellaneda S. A. ; Argentina
Fil: Sial, Alcides. Universidad de Penambuco; Brasil
18th International Sedimentological Congress
International Asociation of Sedimentology
Argentina
Mendoza
https://purl.org/becyt/ford/1.5, EDIACARAN, C-O ISOTOPES, https://purl.org/becyt/ford/1, NEOPROTEROZOIC, TANDILIA SYSTEM
https://purl.org/becyt/ford/1.5, EDIACARAN, C-O ISOTOPES, https://purl.org/becyt/ford/1, NEOPROTEROZOIC, TANDILIA SYSTEM
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