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A 2026 report describes the geology and structural setting of the Regal Ridge emerald property in the Finlayson Lake district of southeastern Yukon. Emerald mineralization is hosted within mid-Paleozoic mafic metavolcanic and metaplutonic rocks and is associated with a 112 Ma quartz monzonite intrusion. The dataset is provided by the Government of Yukon and includes details on host rock chemistry, vein generations, and the relationship between mineralization and Cretaceous deformation.
License is OGL-CA-2.0. File formats are HTML and PDF.