Application of a Passive Surface Wave Method to Estimation of Deep S-wave Velocity Structure in San Francisco Bay Area

Author(s):  
K. Hayashi ◽  
D. Underwood
2013 ◽  
Vol 32 (6) ◽  
pp. 620-626 ◽  
Author(s):  
Koichi Hayashi ◽  
Antony Martin ◽  
Ken Hatayama ◽  
Takayuki Kobayashi

2019 ◽  
Author(s):  
Takayuki Kobayashi ◽  
Takanori Ogahara ◽  
Tomio Inazaki ◽  
Hiroshi Kisanuki ◽  
Chisato Konishi ◽  
...  

2009 ◽  
Vol 118 (3) ◽  
pp. 390-407 ◽  
Author(s):  
Kyosuke ONISHI ◽  
Yoshinori SANADA ◽  
Toshiyuki YOKOTA ◽  
Tomochika TOKUNAGA ◽  
Katsuro MOGI ◽  
...  

Geophysics ◽  
1992 ◽  
Vol 57 (4) ◽  
pp. 653-655
Author(s):  
D. F. Winterstein

What I would like to discuss has little to do with the content of Heloise Lynn’s paper, which beautifully illustrates S‐wave birefringence in near‐surface materials. My concern is with the terminology. Inappropriate use of the term azimuthal anisotropy has become so prevalent in both oral and written presentations that someone needs to point out clearly and in detail why such usage is ill‐advised. My comments, thus, while triggered by the usage of this paper, are for an audience that includes many besides the paper’s author.


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