Lecture Notes on Ore Deposits 101: VMS and Sedex Deposits
Introduction
- Speaker: Andrew Jackson, Economic Geologist at Global Resource Investments
- Objective: Provide understanding of ore deposits for non-technical audiences
- Focus of Lecture: Volcanogenic Massive Sulfides (VMS) and Sedimentary Exhalative (Sedex) deposits
General Concepts
- Metal Concentration Process: Melting of crustal rocks, rise of melt through the crust, concentration of metals
- VMS and Sedex Deposits: Products of sea-floor smokers with different geological settings
Volcanogenic Massive Sulfides (VMS)
- Formation:
- Occur at or near the sea floor
- Copper and zinc-rich, associated with volcanic activity
- Massive sulfide cap on the sea floor, with underlying "feeder" or "Stringer" zone
- Characteristics:
- Often form in clusters over large heat sources
- Found worldwide, significant in copper and zinc production
- Common in geological history, still forming today
- Structure:
- Consist of massive sulfide cap and underlying "Stringer Zone"
- Funnel-shaped neck of fractured rock
- Metal deposition influenced by rapid cooling
- Spatially zoned metals: copper near vents, zinc and lead more distal
- Economic Importance:
- Economically significant, particularly for Canada
- Range in size from 4 to 25 million tons, with some exceptions
- Examples:
- Bisha deposit in Eritrea and Solwara 1 deposit off Papua New Guinea
Sedimentary Exhalative (Sedex) Deposits
- Formation:
- Not directly related to volcanic activity
- Driven by dewatering and metamorphism of sediments
- Lead, zinc, and silver dominant
- Characteristics:
- Form in fault-bounded sedimentary basins
- Generally larger and higher grade than VMS deposits
- Fewer in number
- Economic Importance:
- Major source of lead and zinc
- Range from 1 million to 400 million tons
- Examples:
- Sullivan deposit in British Columbia
Exploration Techniques
- Common Techniques:
- Soil and rock geochemistry
- Electromagnetic geophysics (EM)
- Magnetics and gravity
- Exploration Strategy:
- Identify time breaks in sedimentation
- Focus on stratigraphic sequences and fault zones
- Drill testing based on geophysical and geochemical data
- Example Program: Tarsis's YMD property exploration in Yukon
Key Takeaways
- Both VMS and Sedex are submarine hot spring deposits
- VMS: Volcanic-hosted, copper and zinc, common
- Sedex: Sediment-hosted, zinc and lead, less common but larger
- Exploration uses geophysics and geochemistry extensively
- Future potential for sea-floor mining with high-grade deposits
Conclusion
- Next lecture topic: V vant gold deposits of South Africa, a major source of gold
These notes provide an overview of the geological and economic aspects of VMS and Sedex deposits, key exploration techniques, and examples of significant deposits.