Fluid-Induced Metamorphism and Deformation at the Eastern Boundary of the Sveconorwegian Province
The Sveconorwegian orogen in Scandinavia and the Grenville orogen in Canada are both remnants oflarge and hot orogens that formed part of the supercontinent Rodinia around 1 billion years ago. Formerly deeply buried portions of crust in these orogens are exposed and offer insights into the tectonic dynamics of the basement within large orogens. The Eastern Segment of the Sveconorwegian Province ho