Effect of thermal variations in Mars' mantle on 3D seismic wave propagation

Ebru Bozdag1, Ana-Catalina Plesa2, Sebastiano Padovan2, Nicola Tosil2, Daniel B Peter3, Caio Ciardelli4, Doris Breuer2, Martin Knapmeyer5, Tilman Spohn2, Melanie Drilleau6, Eric Clevede7, Philippe Henri Lognonné6, Jeroen Tromp8, Mark Wieczorek Sr.9, Josh Murphy10, Scott D King11, Benjamin Fernando12, Kuangdai Leng13 and Tarje Nissen-Meyer12, (1)Colorado School of Mines, Golden, CO, United States, (2)German Aerospace Center DLR Berlin, Berlin, Germany, (3)King Abdullah University of Science and Technology, Physical Sciences and Engineering, Thuwal, Saudi Arabia, (4)University of Sao Paulo, Sao Paulo, United States, (5)DLR-Inst Planetary Research, Berlin, Germany, (6)Université de Paris, Institut de physique du globe de Paris, CNRS, Paris, France, (7)Institut de Physique du Globe de Paris, Paris, France, (8)Princeton University, Princeton, NJ, United States, (9)Observatoire de la Côte d'Azur - Laboratoire Lagrange, Nice, France, (10)Virginia Tech, Blacksburg, VA, United States, (11)Virginia Polytechnic Institute and State University, Blacksburg, VA, United States, (12)University of Oxford, Oxford, United Kingdom, (13)University of Oxford, Department of Earth Sciences, Oxford, United Kingdom