The northern limit of the subducted Juan de Fuca plate system

Journal of Geophysical Research: Solid Earth

Volumn 103, Issue B11, 1998, Pages 26949-26961

  Cassidy, John F ^a   Ellis, Robert M ^b   Karavas, Costas ^b   Rogers, Carry C ^a  

^a Geological Survey of Canada Sidney   (Canada)

^b UNIVERSITY OF BRITISH COLUMBIA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

LITHOSPHERIC STRUCTURE; S-WAVE; SEISMIC VELOCITY; SUBDUCTION ZONE; VELOCITY STRUCTURE;

BRITISH COLUMBIA; CANADA; CASCADIA SUBDUCTION ZONE; NORTH AMERICA; VANCOUVER ISLAND;

EID: 0032454514     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: None     Document Type: Article

References (5)

1. Ammon, C.J., The isolation of receiver effects from teleseismic P waveforms, Bull. Seismol. Soc. Am., 81, 2504-2510, 1991.
2. Ammon, C.J., G.E. Randall, and G. Zandt, On the nonuniqueness of receiver function inversions, J. Geophys. Res., 95, 15,303-15,318, 1990.
3. Berteussen, K.A., Moho depth determinations based on spectral ratio analysis of NORSAR long-period P waves, Phys. Earth Planet. Int., 31, 313-326, 1977.
4. Colvert, A.J., and R.M. Clowes, Deep, high-amplitude reflections from a major shear-zone above the subducting Juan de Fuca plate, Geology, 18, 1091-1094, 1990.
5. Cassidy, J.F., Numerical experiments in broadband receiver function analysis, Bull. Seismol. Soc. Am., 82, 1453-1474, 1992.