Discrimination of Thermal versus Mechanical Effects of Shock on Rock Magnetic Properties of Spherically Shocked up to ~10-160 GPa Basalt and Diabase
Natalia S. Bezaeva1,2, Nicholas Swanson-Hysell3, Sonia Tikoo3,4, Dmitry D. Badyukov5, Myriam Annie Claire Kars6, Ramon Egli7, Dmitriy A. Chareev8 and Luke M Fairchild9, (1)Kazan Federal University, Institute of Geology and Petroleum Technologies, Kazan, Russia, (2)Ural Federal University, Institute of Physics and Technology, Yekaterinburg, Russia, (3)University of California Berkeley, Earth and Planetary Science, Berkeley, CA, United States, (4)Rutgers University New Brunswick, New Brunswick, NJ, United States, (5)V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, Russia, (6)University of Plymouth, International Ocean Drilling Programme, Plymouth, UK, (7)Zentralanstalt fuer Meteorologie und Geodynamik, Vienna, Austria, (8)Institute of Experimental Mineralogy RAS, Chernogolovka, Russia, (9)University of California Berkeley, Earth and Planetary Science, Berkeley, United States
