[1]
R. Braga and G. Cinelli, “THE GABBRO AND SERPENTINIZED PERIDOTITE OF BONASSOLA (BRACCO-LEVANTO OPHIOLITE, ITALY) - AN EXTREMELY LOW NATURAL RADIATION AREA TO IMPROVE IN SITU GAMMA SPECTROMETRY”, Ofioliti, vol. 39, no. 2, pp. 43-49, Dec. 2014.