Journal of Geology & Geophysics
Open Access
ISSN: 2381-8719
+44 1478 350008
ISSN: 2381-8719
+44 1478 350008
Trio Fani, Putri Agustin and Heri Nurohman
Posters-Accepted Abstracts: J Geol Geosci
Mount Kendalisodo has a prospect of geothermal. This prospect is assumed by surface geothermal manifestation around this area such as hot springs and altered rocks. Hot spring is analyzed by geochemistry analysis to get some information of chemical fluids characteristic, fluids type, processes that occur with these fluids along it�??s migration from reservoir to surface, and to predict temperature of reservoir. Rocks that are located around Mount Kendalisodo has been analyzed by petrography method to determine minerals exchange. The next tests are carried out to determine the physical properties of rock such as porosity test, permeability test, and density test. There are five hot springs with temperature ranging from 36°C to 40°C and pH value from 5.9-7.8. The hot springs there have a dominant HCO3 composition and it indicates that these fluids are carbonate water with long distance and many process occur during these fluids migration. The hydrothermal alteration influence and site�??s minerals composition with three alteration intensity (secondary minerals composition <25%), medium alteration intensity (secondary minerals composition between 25% and 75%) and high alteration intensity (secondary minerals composition >75%) that changes primary mineral composition to clay mineral in argilic alteration zone. This alteration based of geothermometer analysis, reservoir temperature is 175,190C. So, this system belongs to intermediate entalphy resource.