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- W1573167490 abstract "Abstract The Rio de la Plata Craton (RPC) comprises extensive Neoproterozoic sedimentary successions cropping out mainly in Uruguay and Argentina. The lithostratigraphy and depositional environments of the Las Ventanas, Piedras de Afilar, Cerro Negro and Balcarce formations, and Mina Verdun, Sierras Bayas and Arroyo del Soldado groups is reviewed and summarised. Most of these units were deposited in the Ediacaran, except for the Mina Verdun Group and the lower Sierras Bayas Group, which may be assigned to the late Mesoproterozoic-Tonian. The early Ediacaran Las Ventanas and Playa Hermosa formations are interpreted as rift deposits. The Colombo diamictite in the Sierras Bayas Group is a likely equivalent of the latter units. The Arroyo del Soldado and upper Sierras Bayas Group were deposited in an extensive passive margin developed on the eastern RPC in the late Ediacaran. The Late Ordovician to Early Silurian Balcarce Formation was deposited in an epicontinental, shallow-marine shelf." @default.
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- W1573167490 date "2009-01-01" @default.
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- W1573167490 title "Chapter 4.2 Lithostratigraphy" @default.
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- W1573167490 doi "https://doi.org/10.1016/s0166-2635(09)01605-3" @default.
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