Tsa da Glisza Emerald Occurrence Geological Report

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