Near-surface azimuthal anisotropy using the Rayleigh wave inversion in the Tehran region, Iran
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s10950-023-10169-1.pdf
Reference64 articles.
1. Abbasi A (2019) Linear and nonlinear earthquake location approaches in a case study overview. Phys Earth Planet Inter 293:106265. https://doi.org/10.1016/j.pepi.2019.05.008
2. Abbasi MR, Shabanian E (1999) Fault map of North Tehran. Published by International Institute of Earthquake Engineering and Seismology, Tehran, Iran
3. Abbassi MR, Farbod Y (2009) Faulting and folding in quaternary deposits of Tehran’s piedmont (Iran). J Asian Earth Sci 34(4):522–531. https://doi.org/10.1016/j.jseaes.2008.08.001
4. Abbassi A, Nasrabadi A, Tatar M, Yaminifard F, Abbassi MR, Hatzfeld D, Priestley K (2010) Crustal velocity structure in the southern edge of the Central Alborz (Iran). J Geodyn 49:68–78. https://doi.org/10.1016/j.jog.2009.09.044
5. Adam M-C, Lebedev S (2012) Azimuthal anisotropy beneath southern Africa from very broad-band surface-wave dispersion measurements. Geophys J Int 191:155–174. https://doi.org/10.1111/j.1365-246X.2012.05583.x
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