Moho depth variations and Vp/Vs ratio in the Zagros (Iran) from teleseismic converted waves
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s10950-021-09986-z.pdf
Reference41 articles.
1. Afsari N, Sodoudi F, Taghizadeh-Farahmand F, Ghassemi MR (2011) Crustal structure of Northwest Zagros (Kermanshah) and Central Iran (Yazd and Isfahan) using teleseismic Ps converted phases. J Seismol 15:341–353
2. Al-Lazki AI, Sandvol E, Seber D, Barazangi M, Türkelli N, Mohamad R (2004) Pn tomographic imaging of mantle lid velocity and anisotropy at the junction of the Arabian, Eurasian and African plates. Geophys J Int 158:1024–1040
3. Allen M, Jackson J, Walker R (2004) Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates. TECTONICS 23. https://doi.org/10.1029/2003TC001530
4. Ammon CJ, Randall GE, Zandt G (1990) On the nonuniqueness of receiver function inversions. J Geophys Res 95:15303–15318
5. Berberian M (1994) Master “blind” thrust faults hidden under the Zagros folds: Active basement tectonics and surface morphotectonics. Tectonophysics 241:193–224
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