Regional earthquake location using empirical traveltimes in a region of strong lateral velocity heterogeneity

Author:

Nicholson T.,Clarke D.,Townend J.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference37 articles.

1. New Zealand seismicity: patterns revealed by the upgraded national seismograph network;Anderson;N. Z. J. Geol. Geophys.,1994

2. The 1968 May 23 Inangahua, New Zealand, earthquake: an integrated geological, geodetic, and seismological source model;Anderson;N. Z. J. Geol. Geophys.,1994

3. An intermediate-depth earthquake in the central region of the South Island used to determine a local crustal thickness;Calhaem;N. Z. J. Geol. Geophys.,1977

4. An analysis of the travel times of P waves to North American stations in the distance range 30 degrees to 100 degrees;Cleary;Bull. Seism. Soc. Am.,1966

5. Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions;Demets;Geophys. Res. Lett.,1994

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