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The document discusses the kinematic indicators and fabrics associated with the Finlay-Ingenika fault in British Columbia, characterized by subvertical to vertical faults indicative of dextral transcurrent displacement. It highlights the deformation patterns observed in the region, including the relationship between volcanic and plutonic rocks, and the presence of various structural features such as folds and faults. The study contributes to understanding the geological history and deformation mechanisms in

Author

vishenka

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EN