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Detailed Reference Information |
McGuire, J.J., Zhao, L. and Jordan, T.H. (2000). Rupture dimensions of the 1998 Antarctic Earthquake from low-frequency waves. Geophysical Research Letters 27: doi: 10.1029/1999GL011186. issn: 0094-8276. |
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We inverted frequency dependent phase and amplitude measurements from 1st orbit Rayleigh waves at global stations for the 1st and 2nd degree polynomial moments of the stress-glut rate tensor. The higher moments of the slip-rate distribution determine the fault plane and approximate rupture dimensions. The results show strong rupture propagation to the west with an average velocity of the instantaneous centroid of 3.6¿.1 km/s. The rupture had a characteristic length of 178¿46 km in the east-west direction and a characteristic duration of 48¿2 s. The results are consistent with unilateral rupture on the east-west fault plane of the focal mechanism and rule out significant rupture on the north-south nodal plane. ¿ 2000 American Geophysical Union |
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Abstract |
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Keywords
Seismology, Earthquake dynamics and mechanics, Seismology, Surface waves and free oscillations |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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