Tsa da Glisza Emerald Occurrence Geological Report
Updated 2mo ago
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Description
Emerald mineralization at Tsa da Glisza in southeast Yukon is associated with quartz-tourmaline veins in chromium-rich mafic rocks. A genetic model proposes fluids from magmatic and metamorphic sources mixed, with beryllium from a Cretaceous granite and chromium from surrounding schist. The Government of Yukon published this report on April 17, 2026, detailing exploration methods and implications for regional prospecting.
Use Cases
Identify exploration targets based on the genetic model linking permeable schist and felsic intrusions
Analyze soil geochemistry data for indicators of emerald mineralization
Evaluate drilling and prospecting results from the Tsa da Glisza property
Apply the formulated genetic model to similar geological settings in the region
Strengths
Report includes a detailed genetic model for emerald mineralization
Exploration methods like soil geochemistry, drilling, and prospecting are specified
Published by the Government of Yukon, an authoritative source
Limitations
Column-level documentation is absent; field semantics must be inferred after download
Row count is unknown, which may limit suitability assessment
Data may reflect geographic bias inherent to open_canada
Provenance
Source
Government of Yukon
Collection Method
Geological study and report compilation
Freshness
Last updated 2026-04-17 15:56:16.992660
Geography
Tsa da Glisza property, Finlayson Lake district (NTS 105G/7), Yukon
Data is in HTML and PDF formats; license is OGL-CA-2.0.