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Fluid inclusions from the wels MT-1 and MT-2 in the Mataloko geothermal system were studied microthermom巴tricalyand geochemicaly. The microthermometric data show that homogenization temperatures of the fluid inclusions at the bottom of the well MT-1 are concordant to the thermal structure estimated from other geological and geochemical data of Mataloko. However, those at th巴 bottomof th巴 wellMT 2 ar巴 2030 °C higher than th巴 esti mated pr巴senttemperature (200 °C ). Saliniti巴sof al th巴 fluidinclusions ar巴 V巴rylow. Semi quantitative gas analysis for fluid inclusions from the bottom of th巴 welMT 1 indicates that the inclusions consist mainly of H20 with trace amounts of C02 and CH, . These data imply that the fluid inclusions were probably formed by trapping steam-condensed water at 220-235 °C with smal amounts of the gases at a shalow level in the geothermal system. Comparison of the homogenization temperatures to the boiling point curve of water for th巴 W巴lMT-2 suggests that at least 100 m have be巴n巴rod吋 fromthe Mataloko ar巴asine巴 theg巴oth巴rmalactivity began.

Fluid inclusion study on the wells MT-1 and MT-2 in the Mataloko geothermal system, Indonesia