Shear wave velocity structure of Iranian plateau: using combination of ambient noise cross-correlations (C1) and correlation of coda of correlations (C3)-Reference-Cited by-同舟云学术

Shear wave velocity structure of Iranian plateau: using combination of ambient noise cross-correlations (C1) and correlation of coda of correlations (C3)

Published:2019-06-03 Issue:3 Volume:218 Page:1919-1938
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Ansaripour Mehrdad¹,Rezapour Mehdi¹,Saygin Erdinc²³

Affiliation:

1. Institute of Geophysics, University of Tehran, PO BOX: 14155-6466, Tehran, Iran. E-mail: rezapour@ut.ac.ir

2. Deparment of Physics, School of Physics, Mathematics and Computing, The University of Western Australia, Perth, WA, Australia

3. Deep Earth Imaging, Future Science Platform, CSIRO, Perth, WA, Australia

Funder

Iran National Science Foundation

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggz257/28760228/ggz257.pdf

Reference92 articles.

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3. Transient, synobduction exhumation of Zagros blueschists inferred from P-T, deformation, time, and kinematic constraints: implications for neotethyan wedge dynamics;Agard;J. geophys. Res.: Solid Earth,2006

4. Receiver function inversion by trans-dimensional Monte Carlo sampling;Agostinetti;J. geophys. Int,2010

5. Origin of coda waves: source, attenuation, and scattering effects;Aki;J. geophys. Res,1975

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