Zircon, the mineral most widely used to date rocks by the U-Pb method, is common in crustal rocks, but is increasingly being found in rocks from the upper mantle. Several studies have concluded that this reflects the deep subduction of crustal rocks into the mantle.
This paper presents a new explanation for the presence of crustal zircons in the upper mantle rocks. In this case, granitoid-related melts/fluids, injected into already-emplaced mafic-ultramafic rocks, apparently transported pre-existing zircons and possibly crystallized new grains.