Frequency-dependent anisotropy in Wellington, New Zealand

Geophysical Research Letters

Volumn 24, Issue 24, 1997, Pages 3297-3300

  Marson Pidgeon, Katrina ^a   Savage, Martha Kane ^a  

^a VICTORIA UNIVERSITY OF WELLINGTON   (New Zealand)

Author keywords

[No Author keywords available]

Indexed keywords

ANISOTROPY; POLARIZATION; SEISMIC WAVES; WAVE PROPAGATION; SHEAR FLOW; SHEAR WAVES;

SHEAR WAVE SPLITTING;

SEISMOLOGY; ANISOTROPY;

ANISOTROPY; CRUSTAL STRUCTURE; POLARIZATION; SHEAR WAVE SPLITTING;

NEW ZEALAND, SOUTH ISLAND, WELLINGTON;

AXIS OF SYMMETRY; AZIMUTHAL VARIATIONS; BROADBAND STATION; DOMINANT FREQUENCY; FREQUENCY-DEPENDENT ANISOTROPY; GEOLOGIC STRUCTURES; SHEAR WAVE SPLITTING; WELLINGTON , NEW ZEALAND;

EID: 0031390866     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/97GL03274     Document Type: Article

References (2)

1. Backus, G. E., Long-wave elastic anisotropy produced by horizontal layering. J. Geophys. Res., 67, 4427-4440, 1962.
2. Beanland, S., The North Island dextral fault belt, Hikurangi subduction margin, New Zealand, PhD thesis, 341 pp., Victoria University of Wellington, 1995.