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 (s

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Date: 2016-01-13 05:19:01 Geology 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 (s Add to Reading List Source URL: www.earth.ox.ac.uk Download Document from Source Website File Size: 64,33 KB Share Document on Facebook

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