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Ernest R. Kanasewich

Researcher at University of Alberta

Publications -  70
Citations -  2382

Ernest R. Kanasewich is an academic researcher from University of Alberta. The author has contributed to research in topics: Crust & Seismogram. The author has an hindex of 25, co-authored 70 publications receiving 2286 citations. Previous affiliations of Ernest R. Kanasewich include University of Wyoming.

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Enhancement of Teleseismic Body Phases with a Polarization Filter

TL;DR: In this paper, a time domain polarization filter was used to increase the signal to noise ratio of teleseismic body phases, and the direction of polarization was found from the eigenvector of the largest principle axis.
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LITHOPROBE-southern Vancouver Island: Cenozoic subduction complex imaged by deep seismic reflections: Reply

TL;DR: The LITHOPROBE seismic reflection project on Vancouver Island was designed to study the large-scale structure of several accreted terranes exposed on the island and to determine the geometry and structural characteristics of the subducting Juan de Fuca plate as discussed by the authors.
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Wave propagation in heterogeneous, porous media: A velocity‐stress, finite‐difference method

TL;DR: In this paper, a particle velocity-stress, finite-difference method is developed for the simulation of wave propagation in 2-D heterogeneous poroelastic media, instead of the prevailing second-order differential equations, they consider a first-order hyperbolic system that is equivalent to Biot's equations.
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Lithoprobe crustal reflection cross section of the southern Canadian Cordillera, 1, Foreland thrust and fold belt to Fraser River Fault

TL;DR: In this article, the authors use reflection data from the south central Canadian Cordillera covering the interval from the easternmost metamorphic core complexes near Arrow Lakes to Fraser River fault system along the Fraser River reveal a highly reflective and complex crust.
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Deep Probe: imaging the roots of western North America

TL;DR: In this article, an analysis of the Lithoprobe Deep Probe and Southern Alberta Refraction Experiment data sets, focusing on the region between Deep Probe shots 43 and 55, has resulted in a continental-scale velocity s