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

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

Dec 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000geoji.143..709m&link_type=abstract

Geophysical Journal International, Volume 143, Issue 3, pp. 709-728.

Astronomy and Astrophysics

Astronomy

148

Inversion, Mantle, Mode Coupling, Seismic Structure, Tomography, Waveform Analysis

Scientific paper

We present a 3-D model of shear heterogeneity (Vsh) in the whole mantle, derived from the inversion of hand-picked body, surface and higher-mode waveforms. The forward and inverse problems are formulated using the non-linear asymptotic coupling theory, the zeroth-order asymptotic expansion of a Born seismogram computed by normal mode summation and including coupling across mode branches. We invert iteratively for mantle heterogeneity and for centroid moment tensors until convergence. Our model, SAW24B16, is parametrized 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 boundary layers at low degrees: degrees 5 and 6 near the surface and degree 2 near the core-mantle boundary. The rest of the lower mantle is dominated by degree 3. We find significant heterogeneity up to spherical harmonic degree 24 in the transition zone and the uppermost part of the lower mantle. Our model displays three slow domains extending continuously between uppermost and lowermost mantle, one originating under Africa and two in the Pacific. The results of our modelling also suggest an interaction near the surface 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 Mid-Atlantic Ridge. These anomalies appear to ascend into the upper mantle without altering their shape near the 670km discontinuity. Fast anomalies accumulate near the 670km discontinuity under the Southern Kurile, the Japan trench and the Izu arc, with little or no penetration into the lower mantle, in agreement with results from a variety of regional studies. Cross-sections through subduction zones such as the Marianas, Tonga-Kermadec, Java, the palaeosubduction zone beneath North America and the Peru-Chile trench show continuous fast structures penetrating into the lower mantle, with the depth of penetration varying from region to region. The distribution of both fast and slow anomalies near 670km thus suggests that the discontinuity does not act as a strong barrier to upgoing and downgoing flow between the upper and the lower mantle.

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