scholarly journals The effect of intrinsic oceanic upper-mantle heterogeneity on regionalization of long-period Rayleigh-wave phase velocities

1977 ◽  
Vol 49 (2) ◽  
pp. 357-370 ◽  
Author(s):  
Emile A. Okal
2016 ◽  
Vol 121 (3) ◽  
pp. 1758-1775 ◽  
Author(s):  
David S. Heeszel ◽  
Douglas A. Wiens ◽  
Sridhar Anandakrishnan ◽  
Richard C. Aster ◽  
Ian W. D. Dalziel ◽  
...  

2014 ◽  
Vol 15 (11) ◽  
pp. 4305-4324 ◽  
Author(s):  
Esther K. James ◽  
Colleen A. Dalton ◽  
James B. Gaherty

2010 ◽  
Vol 29 (4) ◽  
Author(s):  
M. CAPUTO ◽  
L. KNOPOFF ◽  
E. MANTOVANI ◽  
St. MUELLER ◽  
G. F. PANZA

1982 ◽  
Vol 72 (4) ◽  
pp. 1329-1349
Author(s):  
H. J. Patton

abstract Single-station measurements of Rayleigh-wave phase velocity are obtained for paths between the Nevada Test Site and the Livermore broadband regional stations. Nuclear underground explosions detonated in Yucca Valley were the sources of the Rayleigh waves. The source phase φs required by the single-station method is calculated for an explosion source by assuming a spherically symmetric point source with step-function time dependence. The phase velocities are used to analyze the Rayleigh waves of the Massachusetts Mountain earthquake of 5 August 1971. Measured values of source phase for this earthquake are consistent with the focal mechanism determined from P-wave first-motion data (Fischer et al., 1972). A moment-tensor inversion of the Rayleigh-wave spectra for a 3-km-deep source gives a horizontal, least-compressive stress axis oriented N63°W and a seismic moment of 5.5 × 1022 dyne-cm. The general agreement between the results of the P-wave study of Fischer et al. (1972) and this study supports the measurements of phase velocities and, in turn, the explosion source model used to calculate φs.


2016 ◽  
Vol 59 (11) ◽  
pp. 2165-2178
Author(s):  
Jian Lü ◽  
ZuJun Xie ◽  
Yong Zheng ◽  
XiaoHui Zha ◽  
Rui Hu ◽  
...  

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