Xe–Ni and Xe–Fe systems are studied in a pressure range relevant to the Earth's core (135–210 GPa) using laser-heated diamond anvil cells and synchrotron X-ray diffraction. The stability of several intermetallic compounds, including XeNi and XeFe, has been recently calculated using structural searches and density functional theory (DFT) above 155 and 190 GPa, respectively [Zhu L, Liu H, Pickard CJ, et al. Nat Chem. 2014;6:644–648]. We have synthesized XeNi around 150 GPa, confirming the prediction; however, it has a cubic -CuAu structure, different from the predicted one for XeNi but identical to the structure predicted for XeFe. -XeNi is calculated to be metastable with DFT. A disordered NiXe () alloy is observed to form prior to this compound. This alloy is interesting in the perspective of a possible storage of xenon in the Earth's core. We have not observed any reaction between Xe and Fe up to 210 GPa.