In situ time-resolved XRD of shock-compressed Fe to 200 GPa
Sovanndara Hok1, Arianna E Gleason2, Cynthia Bolme3, Dylan Rittman4, Sebastien Merkel5, Kyle James Ramos3, Benjamin Morrow3, Timothy Pierce3, Hae Ja Lee6, Bob Nagler6, Eric Galtier6, Eduardo Granados7, Akel Hashim8 and Wendy L Mao9, (1)Stanford University, Department of Geological Sciences, Stanford, CA, United States, (2)SLAC, Menlo Park, CA, United States, (3)Los Alamos National Laboratory, Los Alamos, NM, United States, (4)Stanford University, Geological Sciences, Palo Alto, CA, United States, (5)UMET, Université de Lille, Villeneuve d'Ascq, France, (6)SLAC National Accelerator Laboratory, Menlo Park, United States, (7)CERN European Organization for Nuclear Research, Geneva, Switzerland, (8)University of California Berkeley, Berkeley, CA, United States, (9)Stanford-Geological & Env Sci, Stanford, CA, United States
