LA-ICP-MS Analyses of Sulfides from Gold-Bearing Zones at the Perron Deposit, Abitibi Belt, Canada: Implications for Gold Remobilization through Metamorphism from Volcanogenic Mineralizations to Orogenic Quartz–Carbonate Veins
Abstract
:1. Introduction
2. Regional and Local Geology
3. Gold-Bearing Zones
3.1. Orogenic Gold Mineralization
3.1.1. High-Grade Zone
3.1.2. Grey Cat Zone
3.1.3. Gratien Zone
3.1.4. E2 Gold Zone
3.1.5. N110 Zone
3.2. Primary Volcanogenic-Related Mineralization
3.2.1. Central Polymetallic Zone
3.2.2. Donna Gold–Copper Zone
3.2.3. QF Zone
3.3. Hybrid-Style Mineralization
3.3.1. Team Zone
3.3.2. Upper High-Grade Zone
3.3.3. 210 Zone
3.3.4. Denise Zone
3.3.5. Eastern Denise Zone
4. Material and Methods
5. Results
5.1. Gold Habit and Sulfide Textures
5.2. Pyrite Trace Element Composition
5.3. Sphalerite Trace Element Composition
5.4. Pyrrhotite Trace Element Composition
5.5. Chalcopyrite Trace Element Composition
5.6. Origins of the Various Gold-Bearing Zones
5.7. Comparison of Pyrite and Pyrrhotite
5.8. Comparison of Pyrite with Chalcopyrite and Sphalerite
5.9. Pyrite Signature and Visible Gold
6. Discussion
6.1. Validity of the Classification of Gold-Bearing Zones
6.2. Source for the Gold in Orogenic Gold Mineralization
6.3. Why the HGZ Is So Rich in Gold
6.4. Why Is There an Exceptional Gold Endowment in the Eastern Gold Zone?
7. Conclusions
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Zone | Origin | T °C | Tl | Sn | W | In-Cd-Zn | Bi-Te-Au | Background | Sp | Po | Cpy | New Origin |
---|---|---|---|---|---|---|---|---|---|---|---|---|
QF | Volcanogenic | X | Volc | Volc | Volc | Volc | ||||||
CPZ | Volcanogenic | 382 | X | Volc | Volc | Volc | Volc | |||||
Donna | Volcanogenic | X | Volc | Volc | ||||||||
Grey Cat | Orogenic | 361 | X | Orog | Orog | Volc | Orog- dominated | |||||
HGZ | Orogenic | 364 | X | X | Orog | Orog | Orog | Orog | ||||
E2 | Orogenic | X | X | Orog | Orog- dominated | |||||||
Gratien | Orogenic | 348 | X | Orog | Orog | Orog | ||||||
N110 | Orogenic | 369 | X | Different system | ||||||||
Team | Hybrid | X | X | X | X | X | Orog | Orog | Orog | Orog- dominated | ||
210 | Hybrid | 385 | X | X | X | Different system | ||||||
Upper HGZ | Hydrid | 389 | X | X | Orog | Orog | Orog | Orog- dominated | ||||
Eastern Denise | Hydrid | 373 | X | X | Orog | Orog | Orog | Orog- dominated | ||||
Denise | hybrid | 398 | X | Volc | Volc | Volc | Volc- dominated |
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Gaboury, D.; Genna, D.; Augustin, J.; Bouchard, M.; Trottier, J. LA-ICP-MS Analyses of Sulfides from Gold-Bearing Zones at the Perron Deposit, Abitibi Belt, Canada: Implications for Gold Remobilization through Metamorphism from Volcanogenic Mineralizations to Orogenic Quartz–Carbonate Veins. Minerals 2024, 14, 843. https://doi.org/10.3390/min14080843
Gaboury D, Genna D, Augustin J, Bouchard M, Trottier J. LA-ICP-MS Analyses of Sulfides from Gold-Bearing Zones at the Perron Deposit, Abitibi Belt, Canada: Implications for Gold Remobilization through Metamorphism from Volcanogenic Mineralizations to Orogenic Quartz–Carbonate Veins. Minerals. 2024; 14(8):843. https://doi.org/10.3390/min14080843
Chicago/Turabian StyleGaboury, Damien, Dominique Genna, Jérôme Augustin, Maxime Bouchard, and Jacques Trottier. 2024. "LA-ICP-MS Analyses of Sulfides from Gold-Bearing Zones at the Perron Deposit, Abitibi Belt, Canada: Implications for Gold Remobilization through Metamorphism from Volcanogenic Mineralizations to Orogenic Quartz–Carbonate Veins" Minerals 14, no. 8: 843. https://doi.org/10.3390/min14080843