Receiver function HV ratio: a new measurement for reducing non-uniqueness of receiver function waveform inversion
Author:
Affiliation:
1. State Key Laboratory of Geodesy and Earth's Dynamics, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China. E-mail: chur@asch.whigg.ac.cn
Funder
National Science Foundation of China
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/212/2/1475/22793088/ggx464.pdf
Reference54 articles.
1. The isolation of receiver effects from teleseismic P waveforms;Ammon;Bull. seism. Soc. Am.,1991
2. On the nonuniqueness of receiver function inversions;Ammon;J. geophys. Res.,1990
3. Transdimensional inversion of receiver;Bodin;J. geophys. Res.,2012
4. Empirical relations between elastic wavespeeds and density in the Earth's crust;Brocher;Bull. seism. Soc. Am.,2005
5. Modeling crustal structure through the use of converted phases in teleseismic body-waveforms;Burdick;Bull. seism. Soc. Am.,1977
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