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Geophysical methods can not be separated from how to interpret the image of the subsurface. One of the geophysical methods used to determine the subsurface resistivity distribution is CSAMT (Control Source Audio-Frequency Magneto- telluric). CSAMT is an electromagnetic method that using a grounded e...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/15216 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Geophysical methods can not be separated from how to interpret the image of the subsurface. One of the geophysical methods used to determine the subsurface resistivity distribution is CSAMT (Control Source Audio-Frequency Magneto- telluric). CSAMT is an electromagnetic method that using a grounded electric dipole source. In interpreting the subsurface resistivity distribution is necessary to build the scheme forward modeling and inversion. 1d forward modeling scheme using a horizontally layered earth model and the inversion of 1d using Occam optimization. <br />
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