GEOPHYSICAL JOURNAL INTERNATIONAL, cilt.194, sa.1, ss.534-556, 2013 (SCI-Expanded)
We develop and apply a full waveform inversion method that incorporates seismic data on a wide range of spatio-temporal scales, thereby constraining the details of both crustal and upper-mantle structure. This is intended to further our understanding of crust-mantle interactions that shape the nature of plate tectonics, and to be a step towards improved tomographic models of strongly scale-dependent earth properties, such as attenuation and anisotropy.