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C-O isotopes of the Ediacarian Loma Negra Formation in Barker area, Tandilia System, Argentina: diagenetic implications

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dc.contributorSchwarz, Ernesto
dc.contributorGeorgieff, Sergio Miguel
dc.contributorPiovano, Eduardo Luis
dc.contributorAriztegui, Daniel
dc.creatorGómez Peral, Lucia
dc.creatorSial, Alcides
dc.creatorPoire, Daniel Gustavo
dc.creatorArrouy, Maria Julia
dc.creatorCanalicchio, José
dc.date.issued2010
dc.description.abstractThe 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.
dc.identifierC-O isotopes of the Ediacarian Loma Negra Formation in Barker area, Tandilia System, Argentina: diagenetic implications; 18th International Sedimentological Congress; Mendoza; Argentina; 2010; 398-398
dc.identifier978-987-96296-4-2
dc.identifierhttp://hdl.handle.net/11336/216367
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://naturalis.fcnym.unlp.edu.ar/handle/628872547/56848
dc.languageeng
dc.publisherInternational Asociation of Sedimentology
dc.source18th International Sedimentological Congress: Abstracts Volume
dc.subjectC-O ISOTOPES
dc.subjectNEOPROTEROZOIC
dc.subjectEDIACARAN
dc.subjectTANDILIA SYSTEM
dc.titleC-O isotopes of the Ediacarian Loma Negra Formation in Barker area, Tandilia System, Argentina: diagenetic implications
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeinfo:eu-repo/semantics/conferenceObject
dc.typeinfo:ar-repo/semantics/documento de conferencia
dspace.entity.typePublication

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