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Kadidia and Kadidia Selatan geothermal system are thought to be related to Palu Koro fault activity. This enables the geothermal system to have a high temperature of manifestations and reservoar. Lithology of this area is dominated by granitic type of plutonic rock , with the depresion area filled by surficial deposit. Boiling springs and high temperature hot ground that are found in Kadidia Selatan indicate this system has high temperature of reservoar. This high heat was trigerred by tectonic activity that reheating the possible heat source. The reservoar temperature of this system is

PENENTUAN KESAMAAN RESERVOAR SISTEM PANAS BUMI KADIDIA DAN KADIDIA SELATAN KABUPATEN SIGI, PROVINSI SULAWESI TENGAH BERDASARKAN METODA GEOKIMIA