Variscan suporposition on Ordovician extensional fault-related folds in the Eastern Pyrenees

Puntos clave

• The study uncovers complex fold structures, offering insights into Ordovician geological formations.
• Key evidence shows the interaction of Variscan tectonics with Ordovician extensional faults.
• Observational analysis based on geological mapping and structural interpretation highlights significant stratigraphic relationships.
• These findings may enable further understanding of regional tectonic processes and their geological history.