The structure of the crust and upper mantle to depths of 320 km beneath the Kaapvaal craton, from P wave arrivals generated by regional earthquakes and mining-induced tremors-Reference-Cited by-同舟云学术

The structure of the crust and upper mantle to depths of 320 km beneath the Kaapvaal craton, from P wave arrivals generated by regional earthquakes and mining-induced tremors

Published:2002-11 Issue:4 Volume:35 Page:477-488
ISSN:1464-343X
Container-title:Journal of African Earth Sciences
language:en
Short-container-title:Journal of African Earth Sciences

Author:

Wright C.,Kwadiba M.T.O.,Kgaswane E.M.,Simon R.E.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference32 articles.

1. Velocities in the crust and upper mantle of southern Africa from multimode surface wave dispersion;Bloch;Bulletin of the Seismological Society of America,1969

2. Program to study the crust and mantle of the Archean craton in southern Africa;Carlson;Eos, Transactions of the American Geophysical Union,1996

3. Tomographic study of the upper mantle structure of the South African continent using waveform inversion;Cichowicz;Physics of the Earth and Planetary Interiors,1992

4. Upper mantle structure of southern Africa using Pnl waves;Clouser;Journal of Geophysical Research,1990

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