Reactivated deformation structure induced by Early Cretaceous magmatism in the Sulu Orogen rift basin, eastern China

Key Points

• Reactivated deformation structures signify important geological changes in the Sulu Orogen rift basin.
• Key evidence includes the impact of Early Cretaceous magmatism on regional geological formations.
• Observational analysis of geological samples from the Sulu Orogen reveals critical insights into historical volcanic activity.
• Understanding these geological processes may help predict future tectonic and magmatic activities.