The eastern Waddington thrust belt cuts the eastern margin of the Coast Mountains mid-Cretaceous magmatic arc. Thrust faults carried Triassic rocks of the...
New data on Upper Triassic rocks in the eastern Coast Mountains show that it is Stikinia, not Wrangellia, that lies along the eastern margin of the Coast...
Early Late Cretaceous east-vergent thrusts deform much of the eastern margin of the Coast Plutonic Complex in western British Columbia. Similarities in timing...
This paper documents the newly recognized southern continuation of the early Tertiary Coast shear zone, extending its known length by ~350 km to more than 1200...
Structural and stratigraphic data from the eastern Coast Mountains, British Columbia, point to the presence of a Late Cretaceous thrust belt on the western...
Stratigraphy and structural styles vary greatly in two areas of the Coast Belt near Chilko Lake (Chilcotin Ranges in the east and Coast Mountains in the west)....
Alpine glaciers are efficient agents of erosion and capable of significantly modifying topography. Despite recent advances in theoretical and field studies...
Most metasedimentary rocks in the southern Coast Mountains batholith are of uncertain tectonic affinity because they occur in discontinuous pendants surrounded...
The growth of the Coast Mountains batholith has been documented as episodic through time, and it has become a type example of a continental arc system that...
Périodique (revue)
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