Experimental evidence of sulfide melt evolution via immiscibility and fractional crystallization
Most ore deposits in high-grade metamorphic terranes show signs of remobilization of sulfide ores. During this process the compositions and tenor of the ore change dramatically. In this report we show the results of a study designed to clarify chemical modification of sulfide melts as they cool from high temperatures. Sulfide melts were allowed to "trickle down" through a permeable inert host over an extreme temperature gradient. The effects of crystal fractionation and liquid immiscibility can...[Show more]
|Collections||ANU Research Publications|
|Source:||The Canadian Mineralogist|
|01_Mavrogenes_Experimental_evidence_of_2013.pdf||546.63 kB||Adobe PDF|
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