Seismic reflection and tomographic velocity model constraints on the evolution of the Tofino forearc basin, British Columbia
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/168/2/634/2022242/168-2-634.pdf
Reference39 articles.
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3. The Effect of Fault-bend Folding on Seismic Velocity in the Marginal Ridge of Accretionary Prisms;Cai;Pure Applied Geophys,1995
4. Local thickening of the Cascadia forearc crust and the origin of seismic reflectors in the uppermost mantle;Calvert;Tectonophysics,2006
5. Seismic reflection imaging of two megathrust shear zones in the northern Cascadia subduction zone;Calvert;Nature,2004
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3. Seismic Velocity Structure Beneath the Tofino Forearc Basin Using Full Waveform Inversion;Energies;2021-05-26
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5. Biostratigraphic, strontium isotopic, and geologic constraints on the landward movement and fragmentation of terranes within the Tofino Basin, British Columbia;Canadian Journal of Earth Sciences;2012-07
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