Fig. 6From: Application of in-situ gamma spectrometry for radiogenic heat production estimation in the Western Himalaya, Kohistan, and Karakoram in northern PakistanLithologywise variations in radiogenic heat production (μWm−3) in the study area (a) Nanga Parbat Massif, (b) Kohistan–Ladakh batholith, (c) Karakoram batholithBack to article page