Seismic refraction data in the Gulf of Saint Lawrence: implications for the lower-crustal blocks

A refined model for the wide-angle reflection-refraction profile 88-3 that crosses the foreland basin of the Appalachian orogen is presented. The two major layers of the cratonic crust have velocities of 6.2 and 6.7 km·s -1 with low gradients. Near the exposed North American craton, the 6.7 km·s -1...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Jackson, H R, Marillier, F, Hall, J
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1998
Subjects:
Online Access:http://dx.doi.org/10.1139/e98-043
http://www.nrcresearchpress.com/doi/pdf/10.1139/e98-043