The reduction by hydrogen and the thermal decomposition of a lateritic saprolite nickel ore were studied using the thermogravimetric technique (TGA). The identification of the mineral phases generated after the processing was carried out using X-ray diffraction (XRD) and scanning electron microscopy coupled to a dispersive energy spectrometer (SEM/EDS) techniques. The reduced ore was leached in amoniacal solution and the low value of nickel extraction (≈3 percent) were attributed to the formation of forsterite and enstatite. Thus reduction test were carried out in the presence of chemicals (Na2CO3, NaCl and S8) and the highest extractions values were found for the tests using 10 percent NaCl. Finally, reduction tests on H2 atmosphere in rotary kiln were performed in the presence of NaCl and the product of the reaction was leached in ammoniacal solution. The presence of only 1 percent of NaCl in the furnace increased the nickel extraction values from ≈3 percent to ≈ 90 percent when the experiment was carried out at 850°C. According to the results of X ray diffractometry (XRD) and thermogravimetric analysis (TGA) the presence of NaCl in the system and the reducing atmosphere of H2 promote the segregation of nickel according to the following steps: 1).. Nickel oxide reduction by hydrogen: NiO + H2(g) → Ni + H2O(g). 2) Formation of HCl: Al2SiO5 + 2NaCl + SiO2 + H2O à 2HCl(g) + 2NaAlSiO4. 3). Chlorination of metallic nickel by HCl: Ni + 2HCl(g) → NiCl2 + H2(g). 4). Reduction of nickel chloride by hydrogen: NiCl2 + H2(g) → Ni + 2HCl(g).