The Mineo pallasite is a relatively poorly known meteorite, which shows interesting features that are not fully understood, like the occurrence of iron oxide regions bordering both the olivine grain boundaries and the (Fe,Ni) metal. In this study, the Fe oxides have been characterized by Raman spectroscopy, Electron Microprobe Analysis, Field Emission Scanning Electron Microscopy, Transmission Electron Microscopy (TEM), Energy Dispersive Spectroscopy (EDS) and 3DElectron Diffraction (3D ED). The combination of TEM-EDS and 3D ED yields a reliable identification of the chemical and crystallographic features of the cryptocrystalline portion of the sample. Thus, the Fe-oxides regions were definitely identified as goethite FeO(OH).The occurrence of goethite was unambiguously associated with terrestrial alteration, also confirmed by the presence of calcite, detected by TEM-EDS and 3D ED. Goethite contains minor elements such as Na, Si and Ca likely coming from allumino-silicates in terrestrial environment, and Ni associated with the (Fe, Ni) metal. The observation of goethite along olivine grain boundaries, as alteration product of the (Fe,Ni) metal diagenesis, is also very intriguing as it might be related to the (Fe,Ni) metal intruded into the sub-micrometric olivine fragments during pallasite formation. Further work is needed in order to extensively analyze the texture and composition of olivine/metal boundaries.