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Magnetotelluric survey in the “N” geothermal field was carried out to map the distribution of resistivity value around the “N” geothermal field. The low resistivity value (2 – 10 ohm.m) which overlying the higher resistivity area beneath, usually represents geothermal system cap rocks. This study began with time-series data robust process processingto generate apparent resistivity and phase data from each MT station. 2D inversion model was constructed by using processed MT EDI Files. The final result of this study is a 2D MT model representing the lateral and vertical distribution of geothermal clay cap. Based on this study, cap rock layer was identified by low resistivity distribution (2 Ω.m 10 Ω.m), the medium resistivity layer (11 Ω.m 70 Ω.m) was identified as the transition zone, while high resistivity value (more than 70 Ω.m) represented geothermal reservoir. The existence of a geothermal reservoir around “N” geothermal field was also supported by the occurrence of several manifestations across the area.

Identification of low resistivity layers in the “N” geothermal field using 2D magnetotelluric inversion modelling