Articles | Volume 6, issue 4
The Cryosphere, 6, 909–922, 2012
https://doi.org/10.5194/tc-6-909-2012
The Cryosphere, 6, 909–922, 2012
https://doi.org/10.5194/tc-6-909-2012

Research article 16 Aug 2012

Research article | 16 Aug 2012

Thin-layer effects in glaciological seismic amplitude-versus-angle (AVA) analysis: implications for characterising a subglacial till unit, Russell Glacier, West Greenland

A. D. Booth et al.

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Cited articles

Abercrombie, R. E. and Rice, J. R.: Can observations of earthquake scaling constrain slip weakening?, Geophys. J. Int., 162, 406–424, https://doi.org/10.1111/j.1365-246X.2005.02579.x, 2005.
Aki, K. and Richards, P. G.: Quantitative Seismology, University Science Books, 2nd Ed., 123–144, 2002.
Anandakrishnan, S.: Dilatant till layer near the onset of steaming flow of Ice Stream C, West Antarctica, determined by AVO (amplitude vs. offset) analysis, Ann. Glaciol., 36, 283–286, 2003.
Ayres, A. and Theilen, F.: Preliminary laboratory investigations into the attenuation of compressional and shear waves on near-surface marine sediments, Geophys. Prospect., 49, 120–127, https://doi.org/10.1046/j.1365-2478.2001.00243.x, 2001.
Bakke, N. E. and Ursin, B.: Thin-bed AVO effects, Geophys. Prospect., 46, 571–587, https://doi.org/10.1046/j.1365-2478.1998.00101.x, 1998.
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