Muhammad Syukri, Zul Fadhli, Rosli Saad
The study conducted at Ie-Seu'um geothermal field, Aceh Besar, Aceh (Indonesia), to investigate the flow of hot spring using 2-D resistivity method. Four survey lines using Pole-dipole array was design across the existing hot spring. The 2-D resistivity inversion models show the study area consists of saturated rock, surface water and rock area, which have very low resistivity value that is <5 Ohm.m and expected as hot spring. Hot water flow detected at line L1 and L2 with different depth and distance, and originated from the north part. The most possibility of hot spring flows in Ie-Seu'um are controlled by fault (Seulimuem segment) and expected at >40 m depth © 2014 ejge.
Geophysics Section, Department of Physics, Faculty of Sciences, Syiah Kuala University, Banda Aceh, Indonesia; Geophysics Section, School of Physics, Universiti Sains Malaysia, Penang, 11800, Malaysia
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