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In the magnetotelluric method (MT) the physical parameters measured in the form of resistivity which is the response of a medium that gets electromagnetic waves. Measurement of the response of the electromagnetic waves by measuring the magnitude of the electric field and the magnetic field on the su...
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id-itb.:226962017-09-27T11:45:20Z#TITLE_ALTERNATIVE# MEJER PURBA (NIM : 10212029), JHON Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/22696 In the magnetotelluric method (MT) the physical parameters measured in the form of resistivity which is the response of a medium that gets electromagnetic waves. Measurement of the response of the electromagnetic waves by measuring the magnitude of the electric field and the magnetic field on the surface. Electrical and magnetic field parameters are measured simultaneously which will be used to find out the impedance that the end result can describe the penetration of the electromagnetic field into the earth. The modeling is done using the program algoramma occam 2D. Before modeling the inversion, do the modeling of the future for the next practical purpose first, the future modeling results will then be in inversion with field data to obtain information form resistivity structure beneath the earth's surface. The ultimate goal of the magnetotelluric method is to obtain a subsurface model resistivity distribution close to the actual subsurface condition. text |
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In the magnetotelluric method (MT) the physical parameters measured in the form of resistivity which is the response of a medium that gets electromagnetic waves. Measurement of the response of the electromagnetic waves by measuring the magnitude of the electric field and the magnetic field on the surface. Electrical and magnetic field parameters are measured simultaneously which will be used to find out the impedance that the end result can describe the penetration of the electromagnetic field into the earth. The modeling is done using the program algoramma occam 2D. Before modeling the inversion, do the modeling of the future for the next practical purpose first, the future modeling results will then be in inversion with field data to obtain information form resistivity structure beneath the earth's surface. The ultimate goal of the magnetotelluric method is to obtain a subsurface model resistivity distribution close to the actual subsurface condition. |
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Final Project |
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MEJER PURBA (NIM : 10212029), JHON |
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MEJER PURBA (NIM : 10212029), JHON #TITLE_ALTERNATIVE# |
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MEJER PURBA (NIM : 10212029), JHON |
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MEJER PURBA (NIM : 10212029), JHON |
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https://digilib.itb.ac.id/gdl/view/22696 |
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