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Steep crystalline-basement faults, commonly indicated by
potential-field anomalies, played a crucial role in evolution of
continental cratonic platforms. In the Phanerozoic Western Canada
Sedimentary Province, history of crustal block movements and warps
is reconstructed from the distribution of depocenters, lithofacies
and structures in structural-formational etages in sedimentary
cover. Each etage is a rock succession formed during a particular
tectonic stage; regional tectonic restructuring closes each stage,
and the next stage represents a new tectonic regime. Practical
tectonic analysis, based on observation of rocks and geophysical
data, is a reliable guide for deciphering a region's geologic
history and for resource exploration."
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