Shallow velocity structure above the Socorro Magma Body from ambient noise tomography using the large-N Sevilleta array, central Rio Grande Rift, New Mexico
Nishath Rajiv Ranasinghe1, Lindsay Lowe Worthington2, Brandon Schmandt3, Chengxin Jiang4, Tori S Finlay1, Susan L Bilek5 and Richard C Aster6, (1)University of New Mexico Main Campus, Department of Earth & Planetary Sciences, Albuquerque, NM, United States, (2)University of New Mexico Main Campus, Department of Earth & Planetary Sciences, Albuquerque, United States, (3)University of New Mexico, Department of Earth and Planetary Sciences, Albuquerque, United States, (4)Harvard University, Department of Earth & Planetary Sciences, Cambridge, United States, (5)New Mexico Institute of Mining and Technology, Earth and Environmental Science, Socorro, United States, (6)Colorado State University, Geosciences Department, Fort Collins, United States
