High-resolution evolution of sediment yields in the Valencia and Menorca basins during the Neogene: Relation with climate, tectonics and Ebro Basin opening

Key Points

• Sediment yield in the Valencia and Menorca basins has varied significantly during the Neogene, influenced by various factors.
• Findings include a detailed analysis of sediment yield changes over geological time, suggesting a relationship with climate and tectonic activity.
• Analysis of geological records shows a connection between Ebro Basin opening and sediment dynamics in surrounding regions.
• Understanding these sediment patterns can enhance our knowledge of past climate conditions and geological processes.