X-ray microfl uorescence and EuL 3 micro-X-ray absorption near-edge structure (XANES) spectroscopy were conducted to determine the distribution and valence state of europium in two samples of scheelite (CaWO 4 ) containing between 40 and 350 ppm Eu. The samples come from hydrothermal gold deposits: the Archean Drysdale deposit in Kalgoorlie, Western Australia (DRY1) and the Caledonian, intrusion-related Stepnyak deposit in Kazakhstan (USP31). Laser-ablation ICP-MS analyses reveal that both samples are characterized by bell-shape chondrite-normalized REE patterns with a maximum enrichment around Eu, and a small positive or no Eu anomaly. USP31 displays a complex zoning between this pattern and a strongly LREE-enriched pattern with a strong positive Eu-anomaly. The XANES spectroscopy reveals the coexistence of Eu 2+ and Eu 3+ in both scheelite samples DRY1 and USP31. The oxidation of Eu in USP31 appears to be inhomogeneous within a single crystal, with zones containing a mixture of Eu 2+ and Eu 3+ and zones containing more than 90% Eu 2+ . This study shows that it is possible to obtain semiquantitative element-distribution maps for LREE as well as, in optimal conditions, EuL 3 XANES spectra on a bending magnet beamline equipped with a solid-state detector.