Quantifying Mineral Fabrics in the Coast Plutonic Complex Bella Coola, British Columbia

Abstract

The Coast Plutonic Complex (CPC) of western British Columbia, Canada consists of a long, narrow belt of Jurassic to Eocene granitic to dioritic intrusive rocks that represent more than 100 Ma of nearly continuous subduction-related magmatism. This study investigates deformation within Mesozoic CPC intrusions in the Bella Coola region using field and analytic techniques.