Shear-Wave Velocity Structure of Southern Africa's Lithosphere: Variations in the Thickness and Composition of Cratons and Their Effect on Topography
Author:
Affiliation:
1. School of Cosmic Physics; Geophysics Section, Dublin Institute for Advanced Studies; Dublin Ireland
2. School of Earth Sciences; University College Dublin; Belfield, Dublin Ireland
3. Institut de Physique du Globe; Paris France
Funder
Dublin Institute for Advanced Studies
Science Foundation Ireland
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2017GC007399/fullpdf
Reference139 articles.
1. Adam , J. M.-C. 2013 Seismic structure and anisotropy in southern Africa's lithosphere: Constraints from broad-band surface-wave dispersion
2. Azimuthal anisotropy beneath southern Africa from very broad-band surface-wave dispersion measurements;Adam;Geophysical Journal International,2012
3. Shear wave velocity structure of the southern African upper mantle with implications for the uplift of southern Africa;Adams;Geophysical Journal International,2011
4. Integrated geophysical-petrological modeling of the lithosphere and sublithospheric upper mantle: Methodology and applications;Afonso;Geochemistry, Geophysics, Geosystems,2008
5. Tibetan and Indian lithospheres in the upper mantle beneath Tibet: Evidence from broadband surface-wave dispersion;Agius;Geochemistry, Geophysics, Geosystems,2013
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