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The hosting environment and possible origins and genetic types of the geothermal water in Gushi depression are discussed on the base of isotope characteristics of geothermal water in the study area. The result shows: Isotopes characteristics exists obvious differences in different part of Gushi depression, which indicate their different storage environment, recharge resources and genetic types. Besides infiltration water mixed with modern circulating water which host on an opener thermal environment, residual sedimentary water may be exists in closer geothermal reservoir.