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Magnetic method is one of method in exploration geophysics that usually used for the inital phase of exploration. Magnetic method used based on anomalies or variations of magnetic field due to the variation magnetic behavior of rocks. The variations of measured magnetic field got interpretated as di...
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| Institution: | Institut Teknologi Bandung |
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id-itb.:167472017-09-27T11:45:15Z#TITLE_ALTERNATIVE# JANNAH ( NIM 10205067) pembimbing : Dr. Eng. Alamta Singarimbun, NUR Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/16747 Magnetic method is one of method in exploration geophysics that usually used for the inital phase of exploration. Magnetic method used based on anomalies or variations of magnetic field due to the variation magnetic behavior of rocks. The variations of measured magnetic field got interpretated as distribution of magnetic materials below the surface of the earth. <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> The way to interpret magnetic data is forward modeling by using the polygon talwani method. This method is able to interpret two dimensional cross section of anomalies. The data from observation wich had been done in North of Karangsambung was being interpretated using polygon talwani method and the result is magnetic material with kind of igneous rock as type of granite at a depth of 6 meters on the surface to 48 meters below surface and spread out in 815 meters trajectory. text |
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Magnetic method is one of method in exploration geophysics that usually used for the inital phase of exploration. Magnetic method used based on anomalies or variations of magnetic field due to the variation magnetic behavior of rocks. The variations of measured magnetic field got interpretated as distribution of magnetic materials below the surface of the earth. <br />
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The way to interpret magnetic data is forward modeling by using the polygon talwani method. This method is able to interpret two dimensional cross section of anomalies. The data from observation wich had been done in North of Karangsambung was being interpretated using polygon talwani method and the result is magnetic material with kind of igneous rock as type of granite at a depth of 6 meters on the surface to 48 meters below surface and spread out in 815 meters trajectory. |
| format |
Final Project |
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JANNAH ( NIM 10205067) pembimbing : Dr. Eng. Alamta Singarimbun, NUR |
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JANNAH ( NIM 10205067) pembimbing : Dr. Eng. Alamta Singarimbun, NUR #TITLE_ALTERNATIVE# |
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JANNAH ( NIM 10205067) pembimbing : Dr. Eng. Alamta Singarimbun, NUR |
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JANNAH ( NIM 10205067) pembimbing : Dr. Eng. Alamta Singarimbun, NUR |
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https://digilib.itb.ac.id/gdl/view/16747 |
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