Upper Mantle Structure of Southern Africa from Rayleigh Wave Tomography with 2-D Sensitivity Kernels

Upper Mantle Structure of Southern Africa from Rayleigh Wave Tomography with 2-D Sensitivity Kernels, Figure 2 Figure 2.
Shear-wave velocity profiles at the depths of 50-300 km. A relative low velocity zone appears on all profiles at roughly 160-260 km depths. (a-c) Velocity profiles of AA', BB' and CC' from this study. (d) Shear-wave velocity profile along CC' from the study of Li & Burke (2006). Note the good alignment of the shallow, slow anomaly and the deep, fast anomaly at the distance of 8 degree in (c), which is not well imaged in (d).
<p>
A 3-D shear wave model in southern Africa has been developed from fundamental mode Rayleigh wave phase velocities, which are computed at the period range of 20 to 167 s using a two-plane-wave tomography method. 2-D sensitivity kernels are applied in the phase velocity inversion to account for finite-frequency effects, which are significant at periods greater than 100 s. The new model (Figure 1 and 2) confirms the first-order observations found by Li and Burke [2006], a fast mantle lid extending to ~180 km depth and being underlain by a low velocity zone. One new feature in the model is the vertical alignment of a shallow low velocity anomaly with a deep high velocity anomaly at the western Bushveld province. The alignment makes more sense for interpreting the slow as the result of high iron content from the Bushveld intrusion and the fast as a more depleted residual mantle. A low velocity channel at the depths of 220-310 km from the southern end of the Kheiss belt to the northwest of the Kaapvaal craton is also imaged for the first time. It suggests that the hot asthenosphere outside the craton could migrate into the craton area through a weak channel and thermally erode the cratonic lithosphere from below. In addition, low velocity anomalies from 100 to 180 km agree well with the localities of kimberlites erupted at 65-104 Ma in the Kaapvaal craton, providing additional evidence for the depth extent of mantle xenoliths.
</p><p>References
</p><p>Li, A., and K. Burke (2006), Upper mantle structure of southern Africa from Rayleigh wave tomography, J. Geophys. Res., 111, B10303, doi:10.1029/2006JB004321.
</p><p>Jelsma, H. A., M. J. De Wit, C. Thiart, P. H. Dirks, G. Viola, I. J. Basson, and E. Anckar (2004), Preferential distribution along transcontinental corridors of kimberlites and related rocks of Southern Africa, S. Afr. J. Geol., 107, 301-324.
</p><p>Yang, Y., and D.W. Forsyth (2006), Regional tomographic inversion of amplitude and phase of Rayleigh waves with 2-D sensitivity kernels, Geophys. J. Int., 166, 1148-1160.
</p><p>Acknowledgements: Data used in this study are from the IRIS DMC. Yingjie Yang kindly provided the inversion codes with 2-D sensitivity kernels. This research is supported by NSF grant EAR-0645503.</p>

Comments

No comments yet.

  •  

Welcome

Welcome to the IRIS Image Gallery – a diverse collection of photographs and visuals that encompass the range and breadth of seismology and the seismological community.

Please browse through our albums. These low and medium-resolution images can be freely used for personal and educational/academic purposes, but we request you recognize the image contributor by including in your product or presentation the credit displayed with each image.

More information is available in the Image Use Agreement.

If you have any comments, questions, or suggestions related to the IRIS Image Gallery, you can send them to gallery@iris.edu.

Photo info

Popular tags