Proceedings of the 12th International INQUA meeting on paleoseismology, active tectonic and archaeoseismology

50 PATA Days 2024 A C K N O W L E D G M E N T S The authors thank the support of the Chilean Fondo Nacional de Desarrollo Científico y Tecnológico (FONDECYT), Grant 1240501 and Proyecto PIA/CONICYT Anillo ACT-172002. Kellen Azúa and Sergio Ruiz also thank the Programa de Riesgo Sísmico (PRS), Universidad de Chile. Pablo Salazar was funded by Millennium Institute on Volcanic Risk Research-Ckelar Volcanoes ANID/MILENIO/ICN2021_038 and by Research Center for Integrated Disaster Risk Management (CIGIDEN), ANID/FONDAP/15110017. Fig. 1: Schematic representation to scale of the tomographic model at the central part of the MP (-23.26°), showing the control of the main lithological units recognized on the surface of the MP (Cortés et al., 2007), by the action of the MF from Triassic to Quaternary. The black and segmented lines represent the main faults: Caleta Bandurrias (CBF), Caleta Herradura (CHF), La Rinconcada (LRF), Mejillones (MF), Cerro Gordo (CGF), Aeropuerto (AF), Cerro Fortuna (CFF), Mititus (MF), and Salar del Carmen (SCF) faults. The vertical exaggeration of the geological section is 3x.