Date: 2016-01-13 05:19:01Geology Earth Planetary science Geodynamics Geomorphology Structure of the Earth Seismology Post-glacial rebound Mantle Viscosity Olivine Earthquake | | Project EARTH-16-LH3: Transient deformation of olivine: From seismic wave speeds to glacial isostacy Supervisor: Dr Lars Hansen The deformation behaviour of rocks is a strong function of timescale. On short timescales (sAdd to Reading ListSource URL: www.earth.ox.ac.ukDownload Document from Source Website File Size: 64,33 KBShare Document on Facebook
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