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Inversion of geophysical data is done to obtain the distribution of the physical <br /> <br /> <br /> properties of the subsurface. Results of inversion modeling is regarded as a model <br /> <br /> <br /> that represents the subsurface geologic conditions. Ba...
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id-itb.:205632017-09-27T11:45:17Z#TITLE_ALTERNATIVE# CHAIRONI (NIM : 10210099); Pembimbing : Wahyu Srigutomo, Ph.D, SYAHRUL Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/20563 Inversion of geophysical data is done to obtain the distribution of the physical <br /> <br /> <br /> properties of the subsurface. Results of inversion modeling is regarded as a model <br /> <br /> <br /> that represents the subsurface geologic conditions. Based on the relationship of <br /> <br /> <br /> data and model parameters, inversion modelling grouped into linear inversion and <br /> <br /> <br /> non-linear inversion. In this study, writer do inversion modelling of data <br /> <br /> <br /> magnetotelluric 1-dimensional which the relationship between the data and model <br /> <br /> <br /> parameters are connected by non-linear equations. Magnetotelluric is a method of <br /> <br /> <br /> geophysical exploration that utilizes the electromagnetic naturally waves. Physical <br /> <br /> <br /> parameters that can be searched by this method are resistivity or conductivity of <br /> <br /> <br /> medium. Before inversion modelling, forward modeling is done first by providing <br /> <br /> <br /> model parameter values to get the synthetic data. The synthetic data from forward <br /> <br /> <br /> modelling used in the inversion modeling. This inversion modeling results can be <br /> <br /> <br /> compared with the model parameters given in the forward modeling to evaluate the <br /> <br /> <br /> results of the inversion. This iversion program have used to inversion modelling of <br /> <br /> <br /> real data magnetotelluric with good result. text |
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Inversion of geophysical data is done to obtain the distribution of the physical <br />
<br />
<br />
properties of the subsurface. Results of inversion modeling is regarded as a model <br />
<br />
<br />
that represents the subsurface geologic conditions. Based on the relationship of <br />
<br />
<br />
data and model parameters, inversion modelling grouped into linear inversion and <br />
<br />
<br />
non-linear inversion. In this study, writer do inversion modelling of data <br />
<br />
<br />
magnetotelluric 1-dimensional which the relationship between the data and model <br />
<br />
<br />
parameters are connected by non-linear equations. Magnetotelluric is a method of <br />
<br />
<br />
geophysical exploration that utilizes the electromagnetic naturally waves. Physical <br />
<br />
<br />
parameters that can be searched by this method are resistivity or conductivity of <br />
<br />
<br />
medium. Before inversion modelling, forward modeling is done first by providing <br />
<br />
<br />
model parameter values to get the synthetic data. The synthetic data from forward <br />
<br />
<br />
modelling used in the inversion modeling. This inversion modeling results can be <br />
<br />
<br />
compared with the model parameters given in the forward modeling to evaluate the <br />
<br />
<br />
results of the inversion. This iversion program have used to inversion modelling of <br />
<br />
<br />
real data magnetotelluric with good result. |
format |
Final Project |
author |
CHAIRONI (NIM : 10210099); Pembimbing : Wahyu Srigutomo, Ph.D, SYAHRUL |
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CHAIRONI (NIM : 10210099); Pembimbing : Wahyu Srigutomo, Ph.D, SYAHRUL #TITLE_ALTERNATIVE# |
author_facet |
CHAIRONI (NIM : 10210099); Pembimbing : Wahyu Srigutomo, Ph.D, SYAHRUL |
author_sort |
CHAIRONI (NIM : 10210099); Pembimbing : Wahyu Srigutomo, Ph.D, SYAHRUL |
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https://digilib.itb.ac.id/gdl/view/20563 |
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1821120196263280640 |