Publication 125
How the crust meets the mantle: Lithoprobe perspectives on the Mohorovicic discontinuity and
crust–mantle transition
Frederick A. Cook, Donald J. White, Alan G. Jones, David W.S. Eaton, Jeremy Hall, and Ronald M. Clowes
Abstract
Application of regional geophysical and geological methods throughout two decades of Canada’s Lithoprobe
project provides new opportunities to analyze the Mohorovicic discontinuity (Moho) and crust–mantle transition. The
transect format employed during Lithoprobe, in which 10 specified regions of Canada were targeted for approximately a
decade each, between 1984 and 2003, permitted teams of scientists to focus on geological, geophysical, and tectonic issues
for each transect. As a primary objective was to enhance knowledge of the structure of the crust and lithosphere, an obvious
target in each transect was the nature and origin of the Moho and crust–mantle transition. Accordingly, the combined
results provide new perspectives on the Moho and the relationship of the Moho to the crust–mantle transition. Perhaps the
most important result is that the continental geophysical Moho is a deceptively simple feature; it has a variety of signatures
at different scales that preclude a single, universally applicable interpretation. In methods that provide large-scale information,
such as regional seismic studies, it is a relatively abrupt refraction velocity contrast that often displays a
dramatic downward decrease in seismic reflectivity. However, its origin in a geological or tectonic sense is perhaps best
determined by careful analyses of structural details near the geophysical Moho, which are complex and varied. In some
areas within Canada, it appears that the geophysical Moho may be old and perhaps remains from the time the crust
formed; in other areas, it appears to be a relatively young feature that was superimposed onto older crustal fabrics.
Source
Canadian Journal of Earth Sciences, 47, 315–351, doi: 10.1139/E09-076, 2010.
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