Fig. 19From: Geologic framework of the Fang Hot Springs area with emphasis on structure, hydrology, and geothermal development, Chiang Mai Province, northern ThailandSchlumberger array resistivity soundings from Coothungkul and Chinapongsanond (1985). Low apparent resistivity (< 60 Ωm) occurs in a zone 9–60 m depth on most soundings. Location of soundings shown by the X symbol in Fig. 18Back to article page