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This research article analyzes tidal barforms in the lower Paleozoic Balcarce Formation of Argentina, revealing two distinct types based on sedimentological and architectural characteristics. The study employs virtual outcrop models and sedimentary logs to differentiate between barform–channel types, highlighting their evolution from tide-dominated to tide-influenced settings. The findings contribute to a better understanding of ancient coastal processes and sedimentary structures in deltaic environments.

Author

sara.cristina.memoria

Language

EN