Abstract: Dense and Dry Mantle Between the Continental Crust and the Oceanic Slab: Folding, Faulting and Tearing in the Slab in the Pampean Flat Slab, Southern Central Andes Evidenced by 3D Body Wave Tomography Along the 2015 Illapel, Chile Earthquake Rupture Area (2017 AGU Fall Meeting)

Dense and Dry Mantle Between the Continental Crust and the Oceanic Slab: Folding, Faulting and Tearing in the Slab in the Pampean Flat Slab, Southern Central Andes Evidenced by 3D Body Wave Tomography Along the 2015 Illapel, Chile Earthquake Rupture Area

Diana Comte, Universidad de Chile, AMTC, Santiago, Chile, Marcelo Farías, Universidad de Chile, Departamento de Geología, Santiago, Chile, Steven W Roecker, Rensselaer Polytechnic Inst, Earth & Environmental Sciences, Troy, United States and Mark T Brandon, Yale University, Earth and Planetary Sciences, New Haven, CT, United States

Back to: Multidisciplinary Approaches to Outstanding Questions in Andean Tectonics Posters