Abstract The Trans-Hudson Orogen (THO) of North America is one of the earliest orogens in
Earth's history that evolved through a complete Wilson Cycle. It represents c. 150 Ma of …

Hudson Bay conceals several fundamental tectonic elements of the North American
continent, including most of the ca. 1.9–1.8 Ga Trans-Hudson orogen (THO) and the …

Abstract The northern Canadian Shield is comprised of multiple Archean cratons that were
sutured by the late Paleoproterozoic to form the Canadian component of supercontinent …

In attenuating media, pulse characteristics evolve with propagation distance and saturation
or pressure-dependent changes in rock properties. This nonstationarity of the waveform …

Application of regional geophysical and geological methods throughout two decades of
Canada's Lithoprobe project provides new opportunities to analyze the Mohorovičić …

Three lithospheric cross sections provide a continental-scale synthesis of more than two
decades of coordinated multidisciplinary research during the Canadian Lithoprobe project …

Metamorphic devolatilization is thought to be the critical process that can liberate gold from
amphibolite facies source rocks to form orogenic gold deposits. However, a growing number …

Despite the fact that earthquake occurrence can be strongly influenced by the architecture of
pre‐existing faults, it remains challenging to obtain information about the detailed …

Abstract The Trans-Hudson Orogen (THO), formed from the convergence between the
Superior craton and the composite Churchill Upper Plate (CUP), is one of the best …

The Precambrian lithosphere of western Canada was assembled into the present crustal
configuration between ca. 2.0 1.78 Ga by plate collisions, sometimes accompanied by arc …