Recently, the S receiver function method has been successfully developed to identify upper mantle interfaces. S receiver functions have the advantage of being free of s-wave multiple reflections and can be more suitable than P receiver function for studying mantle lithosphere. However, because of specific ray geometry of the S-to-P converted waves, the S receiver function method has some technical difficulties and limitations. We selected data from teleseismic events (Mb>5.7, epicentral distance between 60?- 85?) recorded since 1996 to present at 8 three component short period stations from the Tabriz Telemetry Network. Clear negative signals from the lithosphere-asthenosphere boundary (LAB) are observed. The average LAB depth is approximately 85 Km and varies from 77 to 103 km underneath the NW of Iran.
Taghizadeh Farahmand, F., Sodoudi, F., Gheitanchi, M. R., & Afsari, N. (2010). The lithosphere-asthenosphere boundary in the North-West of
Iran from S receiver function. Journal of the Earth and Space Physics, 35(4), -.
MLA
Fataneh Taghizadeh Farahmand; Forogh Sodoudi; Mohammad reza Gheitanchi; Narges Afsari. "The lithosphere-asthenosphere boundary in the North-West of
Iran from S receiver function", Journal of the Earth and Space Physics, 35, 4, 2010, -.
HARVARD
Taghizadeh Farahmand, F., Sodoudi, F., Gheitanchi, M. R., Afsari, N. (2010). 'The lithosphere-asthenosphere boundary in the North-West of
Iran from S receiver function', Journal of the Earth and Space Physics, 35(4), pp. -.
VANCOUVER
Taghizadeh Farahmand, F., Sodoudi, F., Gheitanchi, M. R., Afsari, N. The lithosphere-asthenosphere boundary in the North-West of
Iran from S receiver function. Journal of the Earth and Space Physics, 2010; 35(4): -.
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