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Resistivity methods in geothermal exploration activities are used to determine the resistivity of a subsurface layer due to the fluid filled pores of rocks and subsurface temperatures. Resistivity method commonly used in geothermal <br /> <br /> <br /> <br /> <br /...
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| Main Author: | |
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/16291 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Resistivity methods in geothermal exploration activities are used to determine the resistivity of a subsurface layer due to the fluid filled pores of rocks and subsurface temperatures. Resistivity method commonly used in geothermal <br />
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exploration is the method of mise-a-la-masse. This method was chosen because it includes the method of resistivity measurements to map the lateral spread of a conductive below the surface, where in the conductive zone beneath the surface of partially known. By using the Lavenberg-Marquardt inversion can be known to the depth of the resistivity change. The results of the resistivity distribution can be <br />
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used to interpret one dimension data from prospected area of geothermal resources and with this analysis we can identify the main elements of building a geothermal system. |
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