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Olavarría County

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Part of the book series: Springer Earth System Sciences ((SPRINGEREARTH))

Abstract

In the Sierras Bayas Sector clay deposits correspond to the Olavarría Formation and to the Cerro Negro Formation, both of Neoproterozoic age. They represent important sedimentary deposits of the Tandilia System because of their extension and technological applications. The Cerro Largo Formation is spread along the Sierras Bayas area and it consists of three units separated by transitional contacts. Geologic-stratigraphical detail studies led to the redefinition of the unit 3 of the Cerro Largo Formation considering it as a separate unit and named Olavarría Formation, studied in various localities of the Sierras Bayas. The unit is limited by erosive unconformities that separate it from the underlying unit (Cuarcitas Superiores) and the overlying one (Loma Negra Formation). MISS, confirm the presence of algal mats also in the Olavarría Formation. X-ray diffraction, optical, microscopy and SEM have been performed on the clay deposits. At La Pampita quarry, the finding and study of a mud bed—connected to several mud pipes—intercalated in the Loma Negra Formation limestones—are attributed to upward mud injection from the underlying Olavarrıía Formation (telogenesis). In general, the clays have low plasticity index. They have low-refractoriness, and are classified as varied red clays and varied ocher clays. They are used in red ceramics. The Cerro Negro Formation has been found in the subsoil and by the opening of several quarries near the Cerro Negro village. The Cerro Negro Formation was divided in two depositional systems separated by an irregular paleosuperface: the Lower Depositional System and the Upper Depositional System. The mineralogical composition of the clays is different in the two depositional systems. Technological tests have been carried out in “composite” samples (stocks) for each of the depositional systems. The clays of the two depositional systems present similar Pyrometric Cone Equivalent (PCE). They are exploited in the area of Cerro Negro, with excellent results and large reserves, for their use in the manufacture of ceramic floor coverings.

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References

  • Andreis RR, Zalba PE (1989) Estratigrafía y paleogeografía de las secuencias cuarciticas al oeste de Barker (Buenos Aires, Argentina). In: Proceedings of 1° Jornadas Geológicas Bonaerenses, Tandil, pp 909–930

    Google Scholar 

  • Andreis RR, Zalba PE, Iñíguez AM (1992) Paleosuperficies y sistemas depositacionales en el Proterozoico superior de Sierras Bayas, Sistema de Tandilia, Provincia de Buenos Aires, Argentina. In: Proceedings of 4° Reunión Argentina de Sedimentología, vol 1, pp 283–290

    Google Scholar 

  • Andreis RR, Zalba PE, Iñíguez Rodriguez AM, Morosi M (1996) Estratigrafía y evolución paleoambiental de la sucesión superior de la Formación Cerro Largo, Sierras Bayas (Buenos Aires, Argentina). In: Proceedings of 6° Reunión Argentina de Sedimentología, pp 293–298

    Google Scholar 

  • Burley SD, MacQuaker JHS (1992) Authigenic clays, diagenetic sequences and conceptual diagenetic models in contrasting basin-margin and basin-center North Sea Jurassic sandstones and mudstones. In: Houseknecht DW, Pittman ED (eds) Origin, Diagenesis and Petrophysics of Clay Minerals in Sandstones, vol 47. SEPM Special Publication, Tulsa, Oklahoma, USA, pp 81–110

    Google Scholar 

  • Garrido L, Zalba PE, Pereira E (1996) Aplicación tecnológica de arcillas (Acopios) de la sucesión superior de la Formación Cerro Largo, Buenos Aires, Argentina. In: Proceedings of 7° Reunión Argentina de Sedimentología y 1° Simposio de Arcillas, Bahía Blanca, pp 305–310

    Google Scholar 

  • Higgins GE, Saunders JB (1967) Report on 1964 Chatham Mud Island, Erin Bay, Trinidad, West Indies. AAPG Bull 51(1):55–64

    Google Scholar 

  • Iñíguez MA, Zalba PE (1974) Nuevo nivel de arcilitas en la zona de Cerro Negro, partido de Olavarría, provincia de Buenos Aires. LEMIT Serie 2(264):95–100

    Google Scholar 

  • Massabie A, Amos A, Iturriza R (1992) Diapirismo arcilítico tectoinducido, Sierras Bayas, Provincia de Buenos Aires. Rev Asoc Geol Argentina 47(4):389–398

    Google Scholar 

  • Pickering KT, Agar SM, Ogawa Y (1988) Genesis and deformation of mud injections containing chaotic basalt limestone chert associations: examples from the southwest Japan forearc. Geology 16:881–885

    Article  Google Scholar 

  • Poiré DG (1987) Mineralogía y sedimentología de la Formación Sierras Bayas en el núcleo septentrional de las sierras homónimas, Olavarría provincia de Buenos Aires. Tesis Doctoral 494 (inédito). Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, p 271

    Google Scholar 

  • Poiré DG (1993) Estratigrafía del Precámbrico sedimentario de Olavarría Sierras Bayas, provincia de Buenos Aires, Argentina. In: Proceedings of 13° Congreso Geológico Argentino y 3° Congreso de Exploración de Hidrocarburos, Mendoza, vol 2, pp 1–11

    Google Scholar 

  • Sellés Martínez J (1994) Lineamientos estructurales y evolución extensional de la plataforma Neoproterozoica-Eopaleozoica de las Sierras Septentrionales de la Provincia de Buenos Aires (Argentina). Rev Brasil Geocien, Sao Paulo, 2(3):289–295

    Google Scholar 

  • Selley RC (1985) Elements of petroleum geology. W.H. Freeman, San Francisco p 449

    Google Scholar 

  • Von Gosen W, Buggisch W (1989) Tectonic evolution of the Sierras Australes fold and thrust belt (Buenos Aires province/Argentina). Geologisches Rundschau, Stuttgart 79(3):797–821

    Google Scholar 

  • Worden RH, Burley SD (2003) Sandstone diagenesis: the evolution of sand to stone. In: Burley SD, Worden RH (eds) Sandstone diagenesis: recent and ancient. Reprint Series of the International Association of Sedimentologists, Blackwell Publishing Ltd., New York, pp 3–44

    Google Scholar 

  • Zalba PE, Iñíguez AM, Volzone C, Morosi M (1996) Mineralogía y procesos postdeposicionales en la sucesión superior de la Formación Cerro Largo, Sierras Bayas, (Buenos Aires, Argentina). In: Proceedings of 7° Reunión Argentina de Sedimentología y 1° Simposio de Arcillas, Bahía Blanca, pp 299–304

    Google Scholar 

  • Zalba PE, Volzone C, Garrido L, Morosi M, Pereira E (1994) Mineralogical composition and diagenetic processes in the two depositional systems of the Cerro Negro Formation, Buenos Aires, Argentina: industrial application. Rev Geol Chilena 21(2):303–311

    Google Scholar 

  • Zalba PE, Manassero M, Laverret EM, Beaufort D, Meunier A, Morosi M, Segovia L (2007) Middle Permian telodiagenetic processes in Neoproterozoic sequences, Tandilia System, Argentina. J Sediment Res 77:525–538

    Article  Google Scholar 

  • Zalba PE, Morosi ME, Manassero M, Conconi MS (2010) Microscale diagnostic diagenetic features in Neoproterozoic and Ordovician units, Tandilia basin, Argentina: a review. J Appl Sci 10(22):2754–2772

    Google Scholar 

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Correspondence to Patricia Eugenia Zalba .

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Zalba, P.E., Morosi, M.E., Conconi, M.S. (2016). Olavarría County. In: Gondwana Industrial Clays. Springer Earth System Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-39457-2_5

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