Seismic anisotropy in the fore-arc region of the Hikurangi subduction zone, New Zealand
- 1 June 1996
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 95 (3-4) , 211-225
- https://doi.org/10.1016/0031-9201(95)03117-0
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- New Zealand seismicity: Patterns revealed by the upgraded National Seismograph NetworkNew Zealand Journal of Geology and Geophysics, 1994
- A quantitative evaluation of the contribution of crustal rocks to the shear-wave splitting of teleseismic SKS wavesPhysics of the Earth and Planetary Interiors, 1993
- Initial shear wave particle motions and stress constraints at the Anza Seismic NetworkGeophysical Journal International, 1992
- Quantitative measurements of shear wave polarizations at the Anza Seismic Network, southern California: Implications for shear wave splitting and earthquake predictionJournal of Geophysical Research, 1990
- Seismic anisotropy due to preferred mineral orientation observed in shallow crustal rocks in southern AlaskaGeology, 1990
- Shear-wave polarizations near the North Anatolian Fault - III. Observations of temporal changes.Geophysical Journal International, 1987
- Shear-wave splitting in the upper-mantle wedge above the Tonga subduction zoneGeophysical Journal International, 1987
- Shear wave polarization anisotropy in the upper mantle beneath Honshu, JapanJournal of Geophysical Research, 1983
- Subcrustal earthquakes beneath New Zealand; Locations determined with a laterally inhomogeneous velocity modelNew Zealand Journal of Geology and Geophysics, 1977
- A further earthquake at exceptional depth beneath New Zealand (Note)New Zealand Journal of Geology and Geophysics, 1976