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This document summarizes a study of Lake Estanya in northeastern Spain. The lake formed in two connected karstic sinkholes and contains up to 15 meters of sediment fill. Five depositional environments were identified from core samples and characterized by their sedimentary facies. The depositional history over the last 21,000 years involved shifts between brackish and saline conditions driven by climate-influenced hydrological fluctuations. The facies model defined for Lake Estanya provides insight into the

Author

Alejandro

Language

EN