The three-dimensional shear velocity structure of the mantle from the inversion of body, surface and higher-mode waveforms

We present a 3-D model of shear heterogeneity (V-sh) in the whole mantle, d erived from the inversion of hand-picked body, surface and higher-mode wave forms. The forward and inverse problems are formulated using the non-linear asymptotic coupling theory, the zeroth-order asymptotic expansion of a Bor n seismogram computed by normal mode summation and including coupling acros s mode branches. We invert iteratively for mantle heterogeneity and for cen troid moment tensors until convergence. Our model, SAW24B16, is parametrize d laterally in spherical harmonics up to degree 24 and radially in 16 cubic b-splines with knots spaced to reflect the data sampling with depth. The power spectrum of the model is dominated by heterogeneity in the bounda ry layers at low degrees: degrees 5 and 6 near the surface and degree 2 nea r the core-mantle boundary. The rest of the lower mantle is dominated by de gree 3. We find significant heterogeneity up to spherical harmonic degree 2 4 in the transition zone and the uppermost part of the lower mantle. Our model displays three slow domains extending continuously between upperm ost and lowermost mantle, one originating under Africa and two in the Pacif ic. The results of our modelling also suggest an interaction near the surfa ce between the anomalies in the Pacific and the network of mid-ocean ridges in the East Pacific, and between the African anomaly and the low-velocity zone in the Red Sea, the East African Rift, the Mid-Indian Ridge and the Mi d-Atlantic Ridge. These anomalies appear to ascend into the upper mantle wi thout altering their shape near the 670 km discontinuity. Fast anomalies accumulate near the 670 km discontinuity under the Southern Kurile, the Japan trench and the Izu are, with little or no penetration int o the lower mantle, in agreement with results from a variety of regional st udies. Cross-sections through subduction zones such as the Marianas, Tonga- Kermadec, Java, the palaeosubduction zone beneath North America and the Per u-Chile trench show continuous fast structures penetrating into the lower m antle, with the depth of penetration varying from region to region. The distribution of both fast and slow anomalies near 670 km thus suggests that the discontinuity does not act as a strong barrier to upgoing and down going flow between the upper and the lower mantle.