In regionally metamorphosed pelites of the Mount Raleigh pendant, the fibrolite isograd occurs 5km downgrade from the sillimanite isograd. Fibrolite formed...
Early Late Cretaceous east-vergent thrusts deform much of the eastern margin of the Coast Plutonic Complex in western British Columbia. Similarities in timing...
The Scotia-Quaal belt of amphibolite facies metamorphic rocks is in the core of the Coast Plutonic Complex southeast of Prince Rupert, inboard of the Alexander...
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...
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)....
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...
The Coast Plutonic Complex between Prince Rupert and Terrace, British Columbia, developed in two stages between mid-Cretaceous and mid-Eocene time. The early...
Low-temperature thermochronometers are widely used to quantify exhumation histories, typically by interpreting sample cooling age-elevation relationships....
Structural and stratigraphic data from the eastern Coast Mountains, British Columbia, point to the presence of a Late Cretaceous thrust belt on the western...
Périodique (revue)
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