Fluid-filled porosity of magmatic underplates from joint inversion of P and S receiver functions
Author:
Affiliation:
1. Institute of Physics of the Earth, Moscow 123242, Russia. E-mail: vinnik@ifz.ru
2. Instituto Dom Luiz, Universidade de Lisboa, 1749-016 Lisbon, Portugal
Funder
RFBR
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/209/2/961/11044437/ggx067.pdf
Reference35 articles.
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2. Earth-flattening procedure for the propagation of Rayleigh wave;Biswas;Pure appl. Geophys.,1972
3. Crustal structure of the Siberian Craton and the West Siberian Basin: an appraisal of existing seismic data;Cherepanova;Tectonophysics,2013
4. Poisson's ratio and crustal seismology;Christensen;J. geophys. Res.,1996
5. A model for flood volcanism;Cox;J. Petrol.,1980
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1. Crustal structure variations in south-central Mexico from receiver functions;Geophysical Journal International;2019-10-03
2. Crustal Structure in Central‐Eastern Greenland From Receiver Functions;Journal of Geophysical Research: Solid Earth;2019-02
3. CRUST AND MANTLE OF THE BAIKAL RIFT ZONE FROM P- AND S-WAVE RECEIVER FUNCTIONS;Geodynamics & Tectonophysics;2017-01-01
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