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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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| Institution: | Institut Teknologi Bandung |
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id-itb.:162912017-09-27T11:45:08Z#TITLE_ALTERNATIVE# RAMDHANI P (NIM:10206050); Pembimbing : Dr. Eng. Enjang Jaenal Mustopa, LINCOLN Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/16291 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 /> 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 /> <br /> <br /> <br /> <br /> 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. text |
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Indonesia Indonesia |
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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 />
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 />
<br />
<br />
<br />
<br />
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. |
| format |
Final Project |
| author |
RAMDHANI P (NIM:10206050); Pembimbing : Dr. Eng. Enjang Jaenal Mustopa, LINCOLN |
| spellingShingle |
RAMDHANI P (NIM:10206050); Pembimbing : Dr. Eng. Enjang Jaenal Mustopa, LINCOLN #TITLE_ALTERNATIVE# |
| author_facet |
RAMDHANI P (NIM:10206050); Pembimbing : Dr. Eng. Enjang Jaenal Mustopa, LINCOLN |
| author_sort |
RAMDHANI P (NIM:10206050); Pembimbing : Dr. Eng. Enjang Jaenal Mustopa, LINCOLN |
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https://digilib.itb.ac.id/gdl/view/16291 |
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