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

First Page		Document Content
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

	Understanding the value of natural capital on our coast and estuaries • Professor Graham J. C. Underwood • University of Essex Coastal features: result of geomorphology DocID: 1uU60 - View Document
	Geomorphology–116 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph DocID: 1uPeW - View Document
	Erosion, Himalayan Geodynamics, and the Geomorphology of Metamorphism Peter K. Zeitler, Anne S. Meltzer, Department DocID: 1us1W - View Document
	Geomorphology–213 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph DocID: 1tOXZ - View Document
	Bringing Earth Science to Life Earth History Geomorphology Surface Processes DocID: 1trKX - View Document