scholarly journals Seismic attenuation tomography of the Tonga-Fiji region using phase pair methods

1999 ◽  
Vol 104 (B3) ◽  
pp. 4795-4809 ◽  
Author(s):  
Erich G. Roth ◽  
Douglas A. Wiens ◽  
Leroy M. Dorman ◽  
John Hildebrand ◽  
Spahr C. Webb
Keyword(s):  
Seismic Attenuation ◽  
Seismic Attenuation Tomography

scholarly journals High resolution regional seismic attenuation tomography in eastern Tibetan Plateau and adjacent regions

2011 ◽  
Vol 38 (16) ◽  
pp. n/a-n/a ◽  
Author(s):  
Xueyang Bao ◽  
Eric Sandvol ◽  
James Ni ◽  
Thomas Hearn ◽  
Yongshun John Chen ◽  
...  
Keyword(s):  
High Resolution ◽  
Tibetan Plateau ◽  
Seismic Attenuation ◽  
Eastern Tibetan Plateau ◽  
Seismic Attenuation Tomography

Seismic attenuation tomography in frequency domain and its application to engineering

2000 ◽  
Vol 43 (4) ◽  
pp. 431-438 ◽  
Author(s):  
Yonggui Zhao ◽  
Qin Li ◽  
Hong Guo ◽  
Hongxiao Jin ◽  
Chaofan Wang
Keyword(s):  
Frequency Domain ◽  
Seismic Attenuation ◽  
Seismic Attenuation Tomography

scholarly journals Ambient noise Love wave attenuation tomography for the LASSIE array across the Los Angeles basin

2021 ◽  
Vol 7 (22) ◽  
pp. eabe1030
Author(s):  
Xin Liu ◽  
Gregory C. Beroza ◽  
Lei Yang ◽  
William L. Ellsworth
Keyword(s):  
Los Angeles ◽  
Wave Attenuation ◽  
Plate Boundary ◽  
Seismic Attenuation ◽  
Supplementary Information ◽  
Los Angeles Basin ◽  
The North ◽  
Attenuation Structure ◽  
Earthquake Faults ◽  
Seismic Attenuation Tomography

The Los Angeles basin is located within the North America–Pacific plate boundary and contains multiple earthquake faults that threaten greater Los Angeles. Seismic attenuation tomography has the potential to provide important constraints on wave propagation in the basin and to provide supplementary information on structure in the form of the distribution of anelastic properties. On the basis of the amplitude information from seismic interferometry from the linear LASSIE array in the Los Angeles basin, we apply station-triplet attenuation tomography to obtain a 2D depth profile for the attenuation structure of the uppermost 0.6 km. The array crosses four Quaternary faults, three of which are blind. The attenuation tomography resolves strong attenuation (shear attenuation Qs ~ 20) for the fault zones and is consistent with sharp boundaries across them.

A robust and accurate seismic attenuation tomography algorithm

2011 ◽  
Author(s):  
Wenyi Hu ◽  
Jonathan Liu ◽  
Lorie Bear ◽  
Carey Marcinkovich
Keyword(s):  
Seismic Attenuation ◽  
Seismic Attenuation Tomography
Sign in / Sign up

Export Citation Format

Share Document