HAL (France)
open access
Deciphering Melt Percolation through Mantle Microstructures: Evidence from Oman Harzburgites
Reactive porous flow and melt–rock interaction are fundamental processes in the evolution of the oceanic lithospheric mantle. Melt migration through reactive porous flow in the Oman ophiolite has been extensively studied in the context of focused melt flow, leading to the formation of dunite channel
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