Rifting mechanisms constrained by InSAR, seismicity, GPS, and surface rupture from the Karonga earthquake sequence in northern Lake Malawi (Nyasa)
Matthew E Pritchard1, Whyjay Zheng2, Scott T Henderson3, James B Gaherty4, Donna J Shillington4, Sarah Jaye C Oliva5, Cynthia J Ebinger6, Scott L Nooner7, Julie Elliott8, Elifuraha Saria9, Daud Ntambila9 and Patrick Rafiki N Chindandali10, (1)Cornell University, Earth and Atmospheric Sciences, Ithaca, NY, United States, (2)National Central University, Center for Space and Remote Sensing Research, Kanagawa, Japan, (3)University of Washington, Earth and Space Sciences, Seattle, United States, (4)Columbia University, Lamont-Doherty Earth Observatory, Palisades, NY, United States, (5)Tulane University of Louisiana, New Orleans, United States, (6)Tulane University, School of Science & Engineering, New Orleans, United States, (7)University of North Carolina at Wilmington, Dept of Earth and Ocean Sciences, Wilmington, NC, United States, (8)Michigan State University, Earth and Environmental Sciences, East Lansing, MI, United States, (9)Ardhi University, Dar Es Salaam, Tanzania, (10)Northern Arizona University, School of Earth and Sustainability, Flagstaff, AZ, United States
