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Volcano-sedimentary megaclast in Wernecke breccia, Yukon, and its bearing on...

A group of hydrothermal breccias, collectively known as Wernecke breccia, formed at approximately 1.60 Ga in Yukon. The breccias consist of a hydrothermally precipitated matrix...

Date updated: 2011-04-04

Date created: 2011-04-04

Publisher: Yukon Geological Survey

Format: HTML
Paleoproterozoic Bonnet Plume River intrusions: Evidence for a calc-alkaline...

The 1.71 Ga Bonnet Plume River intrusions (BPRI) and related volcanics are preserved only as clasts in the 1.60 Ga Wernecke breccias of Yukon that host iron-oxide copper gold...

Date updated: 2011-04-04

Date created: 2011-04-04

Publisher: Yukon Geological Survey

Format: HTML

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The Government of Yukon acknowledges that Indigenous Peoples have traditional territories throughout the Yukon and celebrates their role as stewards of the lands and waters and their ongoing connection to this place.