Abstract
ALTHOUGH the use of seismic arrays for direct measurement of P wave travel time gradients (d T/dΔ) has greatly improved the resolution of upper mantle structure1–3, the technique is limited by the effects of local crustal structure beneath arrays and by the paucity of events giving arrivals of sufficient quality for dT/dΔ measurements. Using the Australian array WRA, we find that the combination of a large quantity of travel time data with selected dT/dΔ measurements provides a more powerful tool for the interpretation of P wave arrivals than either technique used in isolation.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
We are sorry, but there is no personal subscription option available for your country.
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Johnson, L. R., J. Geophys. Res., 72, 6309 (1967).
Kanamori, H., Bull. Earthquake Res. Inst. Tokyo Univ., 45, 657 (1967).
Niazi, M., and Anderson, D. L., J. Geophys. Res., 70, 4633 (1965).
Cleary, J. R., Wright, C., and Muirhead, K. J., Geophys. J., 16, 21 (1968).
Wright, C., thesis, Australian National Univ. (1970).
Wright, C., Earth Planet, Sci. Lett., 8, 41 (1970).
Archambeau, C. B., Flinn, E. A., and Lambert, D. G., J. Geophys. Res., 74, 5825 (1969).
Green, R. W. E., and Hales, A. L., Bull. Seism. Soc. Amer., 58, 267 (1968).
Whitcomb, J. H., and Anderson, D. L., J. Geophys. Res., 75, 5713 (1970).
Anderson, D. L., Science, 157, 1165 (1967).
Ringwood, A. E., Phys. Earth Planet. Interiors, 3, 109 (1970).
Ringwood, A. E., in The Earth's Crust and Upper Mantle, Geophys. Monog. (edit, by Hart, P. J.), 13, 1 (American Geophysical Union, Washington, 1969).
Toksöz, M. N., Minear, J. W., and Julian, B. R., J. Geophys. Res., 76, 1113 (1971).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
SIMPSON, D., WRIGHT, C. & CLEARY, J. Double Discontinuity in the Upper Mantle. Nature Physical Science 231, 201–203 (1971). https://doi.org/10.1038/physci231201a0
Received:
Issue Date:
DOI: https://doi.org/10.1038/physci231201a0
This article is cited by
-
Slowness and azimuth at the Uppsala array
Pure and Applied Geophysics (1973)