| Title | Resistivity Structure of Puga Geothermal Field |
|---|---|
| Authors | R.P. Singh and S. Nabetani |
| Year | 1995 |
| Conference | World Geothermal Congress |
| Keywords | Puga valley, magnetotelluric method, resistivity structure, GEMIT method |
| Abstract | The magnetotelluric recordings at locations have been camed at Puga geothermal field. Five components of the electric and magnetic fields have been recorded at each stations. The electric field components have been found very noisy at each stations. In order to infer the resistivity structure from the noisy magnetotelluric data, the Geoelectromagnetic Induction Tomography (GEMIT) technique (Nabetani 1987) has been used. In the present paper, we present the results terms of twodimensional map of the electrical resistivity structure inferred only from magnetic fields. The depth of the geothennal reservoir and the extent ofthe geothermal reservoir have been discussed in view ofthe resistivity from the magnetotelluric recodings. |