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Web under the right conditions of low oxidation, diamonds can form in the convecting mantle, the subducting slab, and the mantle keel. Web diamond bearing rock (kimberlite) showing dark crystals (olivine) and fragments of rock formed during. Web diamonds form from fluids in the mantle that migrate due to plate tectonics diamond is a metasomatic mineral that. Web a new laboratory experiment finds that, under extreme temperatures and pressures, the combination of iron, carbon.