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The discharge fluid in a single vapor phase from the exploration well MT-2, drilled to a depth of 162.35 m in the Mataloko geothermal field, Flores Island, Indon巴sia,is relatively low in non-condensable gas content (0.61 -0.69 wt%) and its gas component is predominant in C02 (91 mole%). The discharge steam is thought to be derived from a liquid water dominat巴d res巴rvoir巴xistingat a deeper l巴V巴l Isotopic compositions of hydrog巴n,oxyg巴n,carbon, sulfur and helium, and chemical composition of minor gas巴sin the discharg巴 fluidfrom th巴 wellMT 2 suggest that its water vapor (H20) consists of mainly m抗日oricwater affected by magmatic water or water四 rockinteraction, while the gaseous components originate mainly from magmatic fluid. Based on several chemical and isotopic geothermometers and measured bore hole temperatures of the wel MT-2, the subsurface temperature is estimated to be 192 -230 °C at the shalow st巴am-dominat巴dr巴servoirand 270 -306 °C at th巴 deepwater-dominat巴dr巴servoir.Th巴 discharg巴 steam from th巴巴xplorationw巴1MT-1 and fumaroles, which ar巴 locatedwithin 200 m from w巴1 MT-2, shows ch巴micalcharacteristics similar to well MT-2. It sugg巴ststhat th巴yare deriv日d from a common source, that is a deep water-dominated reservoir possibly having a relatively large extension in the Mataloko field.

Chemical and isotopic studies of well discharge fluid of the Mataloko geothermal field, Flores, Indonesia