Fig. 5From: Radiogenic heat production in granitoids from the Sierras de Córdoba, Argentina a A (µW/m3) vs. SiO2 content (%) for each intrusion. b A (µW/m3) vs. K (%) for the different lithologic types. c A (µW/m3) vs. Th (ppm) for the different lithologic types. d A (µW/m3) vs. U (ppm) for the different lithologic typesBack to article page