Karaha-Telaga Bodas is a recently discovered geothermal system located adjacent to Galunggung Volcano in western Java. Drilling to depths of 3 km has documented an extensive vapor-dominated zone and a deeper liquid reservoir with measured temperatures up to 350oC and salinities of 1-2 weight percent.

The vein parageneses record the evolution of a high temperature liquid-dominated system that developed before the onset of vapor-dominated conditions. The change to a vapor-dominated regime was marked by the deposition of chalcedony and quartz. Fluid inclusions trapped in quartz and the mineral relationships indicate that the pressure gradients at the start of this change greatly exceeded hydrostatic and that much of the chalcedony was deposited at temperatures >250oC. The deposition of chalcedony at these temperatures implies catastrophic depressurization and boiling of the reservoir liquids.

As pressures within the reservoir declined, downward percolating steam condensate deposited anhydrite, calcite, fluorite, pyrite, and chlorite. At depths greater than 800 m, boiling off of the condensate resulted in increasing salinities with increasing temperature. Hypersaline fluids with salinities of 31 weight percent NaCl equivalent were trapped at 300oC in anhydrite. Rock surfaces were subsequently coated with scales of NaCl, KCl, FeClx, and Ti-Si-Fe as the condensate boiled to dryness.

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Copyright 2002, Stanford Geothermal Program: Readers who download papers from this site should honor the copyright of the original authors and may not copy or distribute the work further without the permission of the original publisher.