Volcanic architecture and three-dimensional alteration model for the Wolverine VMS Deposit, Yukon

火山成因的锌铜铅块状硫化物矿床在加拿大制造业所用金属中占很大比例，对加拿大的经济成功至关重要。 Finlayson湖区的金刚狼火山岩型块状硫化物存款是在育空地区东南部新发现的此类存款，可能在未来几年内投入生产。 该项目旨在了解该存款中岩石的关系和几何形状，以便重建与金刚狼存款空间相关的古代海底火山。 此外，该项目将利用实地方法和岩石及矿物的化学分析研究海水-岩石相互作用的性质。 该项目的结果将提供工具，将增加我们的知识和能力，以寻找这些存款都在芬莱森湖区，在加拿大和世界其他地方。

Zinc-copper-lead volcanogenic massive sulphide (VMS) deposits provide a significant proportion of the metals used in the Canadian manufacturing sector and are critical to the economic success of Canada.  The Wolverine volcanic-hosted massive sulphide deposit of the Finlayson Lake district is a newly discovered deposit of this type in southeastern Yukon and will likely enter into production in the next few years.  This project is aimed at understanding the relationship and geometry of the rocks in this deposit in order to reconstruct the ancient undersea volcano that is spatially associated with the Wolverine deposit.  In addition, this project will study the nature of seawater-rock interaction using field methods and chemical analysis of rocks and minerals.  The results of this project will provide tools that will increase our knowledge and ability to search for these deposits both in the Finlayson Lake district, and elsewhere in Canada and the world.