Rock magnetic effects induced in terrestrial basalt and diabase by >20 GPa experimental spherical shock waves
Natalia S. Bezaeva1,2, Nicholas Swanson-Hysell3, Sonia Tikoo3, Dmitry D. Badyukov4, Myriam Annie Claire Kars5, Ramon Egli6, Dmitriy A. Chareev7, Luke M Fairchild8, Evgeniya Khakhalova9, Becky E Strauss9 and Anna K. Lindquist10,11, (1)Ural Federal University, Institute of Physics and Technology, Yekaterinburg, Russia, (2)Kazan Federal University, Institute of Geology and Petroleum Technologies, Kazan, Russia, (3)University of California Berkeley, Earth and Planetary Science, Berkeley, CA, United States, (4)V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, Russia, (5)Kochi University, Center for Advanced Marine Core Research, Nankoku, Japan, (6)Zentralanstalt fuer Meteorologie und Geodynamik, Vienna, Austria, (7)Institute of Experimental Mineralogy RAS, Chernogolovka, Russia, (8)University of California Berkeley, Earth and Planetary Science, Berkeley, United States, (9)Institute for Rock Magnetism, University of Minnesota, Minneapolis, MN, United States, (10)Lake Superior State University, Department of Geology and Physics, Sault Ste Marie, MI, United States, (11)University of Arkansas, Department of Geosciences, Fayetteville, AR, United States
