Carbonated magmatic sulfide systems: Still or sparkling?
Maria Cherdantseva1, Michael Anenburg2, Marco Fiorentini1
1Centre for Exploration Targeting, School of Earth Sciences, The University of Western Australia, 35 Stirling Hwy, 6009 Crawley, Perth, WA, Australia.
Carbonate melt interaction with sulfide liquid offers a new explanation for metal-rich sulfide transport in mafic magmas. This finding is key to understanding the origin of essential nickel, copper, and platinum-group element resources.
Area of Science:
- Geochemistry
- Economic Geology
- Magma Dynamics
Background:
- The transport of dense metal-rich sulfide liquid within mafic magmas is a long-standing debate.
- Understanding this process is vital for locating nickel, copper, and platinum-group element (PGE) resources essential for sustainable energy.
Purpose of the Study:
- To investigate the mechanism of metal-rich sulfide liquid transport in mafic magmas.
- To propose and experimentally validate an alternative hypothesis for long-distance sulfide transport.
Main Methods:
- Experimental petrology to simulate magma-sulfide-carbonate interactions.
- Microscopic and textural analysis of experimental products.
Main Results:
- Observed that carbonate melt wraps around sulfide globules.
- This carbonate-sulfide interaction forms a mobile phase capable of transport.
- The proposed mechanism contrasts with previous gas-bubble hypotheses.
Conclusions:
- Carbonate melt plays a crucial role in mediating the transport of metal-rich sulfide liquids.
- This interaction facilitates sulfide migration from the mantle to the crust.
- The findings provide a new framework for understanding the genesis of magmatic ore deposits.
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