Evidence for underthrusting beneath the Queen Charlotte Margin, British Columbia, from teleseismic receiver function analysis

Geophysical Journal International

Volumn 171, Issue 3, 2007, Pages 1198-1211

  Bustin, A M M ^a,b,c   Hyndman, R D ^a,b   Kao, H ^b   Cassidy, J F ^b  

^a UNIVERSITY OF VICTORIA   (Canada)

^b Geological Survey of Canada Sidney   (Canada)

^c UNIVERSITY OF BRITISH COLUMBIA   (Canada)

Author keywords

Inversion; Plate boundary; Queen Charlotte Margin; Receiver function; Seismic structure; Subduction; Underthrusting

Indexed keywords

CONTINENTAL MARGIN; CRUSTAL DEFORMATION; CRUSTAL THICKENING; FAULT ZONE; INVERSE ANALYSIS; MODELING; NORTH AMERICAN PLATE; OCEANIC CRUST; PACIFIC PLATE; PLATE BOUNDARY; PLATE CONVERGENCE; SEISMOLOGY; SUBDUCTION; TELESEISMIC WAVE; THRUST;

BRITISH COLUMBIA; CANADA; NORTH AMERICA; QUEEN CHARLOTTE ISLANDS;

EID: 36348981649     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2007.03583.x     Document Type: Article

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