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Download Volume II Accomplisments (28 Mb pdf). - IRIS

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S-Velocity Structure of the Upper Mantle<br />

Sergei Lebedev (Dublin Institute for Advanced Studies), Rob D. van der Hilst (MIT)<br />

Sv-velocity structure of the upper mantle<br />

(crust–660 km) is constrained by the Automated<br />

Multimode Inversion of surface and S-wave forms<br />

[Lebedev et al., 2005], applied to a large global<br />

data set retreived from <strong>IRIS</strong> facilities [Lebedev<br />

and van der Hilst, 2008]. Structure of the mantle<br />

and crust is constrained by waveform information<br />

from both the fundamental mode Rayleigh waves<br />

(periods from 20 to 400 s) and S and multiple S<br />

waves (higher modes). The reference model used<br />

in the waveform inversions and the tomographic<br />

linear inversion incorporates 3-D crustal structure.<br />

The tomographic model includes isotropic<br />

variations in S- and P-wave velocities and also<br />

S-wave azimuthal anisotropy. The lateral resolution<br />

of the imaging is a few hundred kilometres,<br />

varying with data sampling.<br />

The technique has been benchmarked with a<br />

‘spectral-element’ resolution test: inverting published<br />

global synthetic data sets computed with<br />

the spectral-element method for laterally heterogeneous<br />

mantle models, Lebedev and van der<br />

Hilst [2008] have been able to reconstruct the<br />

synthetic models accurately.<br />

The tomographic model displays low-Sv-velocity<br />

anomalies beneath mid-ocean ridges and backarc<br />

basins that extend down to ~100 km depth<br />

only. In the seismic lithosphere beneath cratons,<br />

strong high velocity anomalies extend to ~200<br />

km. Pronounced low-velocity zones beneath cratonic<br />

lithosphere are rare; where present (South<br />

America; Tanzania) they are often neighboured<br />

by volcanic areas near cratonic boundaries. The<br />

images of these low-velocity zones may indicate<br />

hot material possibly of mantle-plume origin—<br />

trapped or spreading beneath the thick cratonic<br />

lithosphere [Lebedev and van der Hilst, 2008].<br />

Cross-section depths and color-scale limits are specified within each frame. The reference<br />

Sv-wave velocity values are, for increasing depths: 4.38, 4.39, 4.69, 5.27 km/s—all at a reference<br />

period of 50 s.<br />

References<br />

Lebedev, S., G. Nolet, T. Meier, R. D. van der Hilst, Automated multimode inversion of surface and S waveforms, Geophys. J. Int. 162, 951-964,<br />

2005.<br />

Lebedev, S., R. D. van der Hilst, Global upper-mantle tomography with the automated multimode inversion of surface and S-wave forms,<br />

Geophys. J. Int., 173, 505-518, 2008.<br />

2010 <strong>IRIS</strong> Core Programs Proposal | <strong>Volume</strong> <strong>II</strong> | Upper Mantle Structure and Dynamics | <strong>II</strong>-169

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