Subsurface Structure and Fluid Flow Analyses Using Geophysical Methods in Geothermal Manifestation Area of Paguyangan, Brebes, Central Java']Java

The indication of an active geothermal system is shown by the presence of surface manifestations such as the hot spring in Kedungoleng, Paguyangan, Brebes, Central Java. The temperature of the largest hot spring reaches 74 degrees C and there is an assumption that this is an outflow of Mount Slamet geothermal system. Purposing to understand the subsurface structure around manifestation, DC- resistivity method had been applied. While Spontaneous Potential ( SP) and Shallow Surface Temperature surveys were conducted to determine the thermal fluid flow pattern and its correlation the distribution shallow surface temperature respectively. The subsurface resistivity has been investigated using 5 points of the Schlumberger configuration with 400 m separation for each point. For the fluid and temperature pattern, a measurement using 15 m interval in 3 lines of conducting fixed electrode configuration has been carried out, along with a 75 cm of depth of temperature measurement around the manifestation area. The thermal fluid is assumed by the low resistivity of 0.756 to 6.91 Omega m and this indicates sandstone that has permeable characteristic. The fluid flows in two layers of Sandstone at more than 10 meter from surface of the first layer. The SP values, which is voltage ( electrical potential) gradients along measurement lines, have a range between - 11- 11 mV and a depth interval of 13.4228.75 m and the distribution of temperature is between 24 degrees- 70 degrees C at a tilting range of 46.06 degrees- 12.60 degrees. Hence it can be inferred that the thermal fluid moves in the Northwest direction and is controlled by a fault structure stretching from Northwest to Southeast.