2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network
In this paper, two modeling method are employed. First, a method based on the Marquardt’s algorithm is presented to invert the gravity anomaly due to a finite vertical cylinder source. The inversion outputs are the depth to top and bottom, and radius parameters. Second, Forced Neural Networks (FNN)...
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General Directorate of Mineral Research and Exploration
2020-04-01
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doaj-1f739b6d86ac44088ed69c8b2ffa070b2020-11-25T02:23:36ZengGeneral Directorate of Mineral Research and ExplorationBulletin of the Mineral Research and Exploration0026-45632020-04-01161161334710.19111/bulletinofmre.589224762D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural networkAta ESHAGHZADEHSanaz SEYEDI SAHEBARIAlireza DEHGHANPOURIn this paper, two modeling method are employed. First, a method based on the Marquardt’s algorithm is presented to invert the gravity anomaly due to a finite vertical cylinder source. The inversion outputs are the depth to top and bottom, and radius parameters. Second, Forced Neural Networks (FNN) for interpreting the gravity field as try to fit the computed gravity in accordance with the estimated subsurface density distribution to the observed gravity. To evaluate the ability of the methods, those are employed for analyzing the gravity anomalies from assumed models with different initial parameters as the satisfactory results were achieved. We have also applied these approaches for inverse modeling the gravity anomaly due to a Chromite deposit mass, situated east of Sabzevar, Iran. The interpretation of the real gravity data using both methods yielded almost the same results.http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/589224?publisher=mtachromite depositforced neural networksmarquardt’s algorithmfinite vertical cylindergravity |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ata ESHAGHZADEH Sanaz SEYEDI SAHEBARI Alireza DEHGHANPOUR |
spellingShingle |
Ata ESHAGHZADEH Sanaz SEYEDI SAHEBARI Alireza DEHGHANPOUR 2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network Bulletin of the Mineral Research and Exploration chromite deposit forced neural networks marquardt’s algorithm finite vertical cylinder gravity |
author_facet |
Ata ESHAGHZADEH Sanaz SEYEDI SAHEBARI Alireza DEHGHANPOUR |
author_sort |
Ata ESHAGHZADEH |
title |
2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network |
title_short |
2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network |
title_full |
2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network |
title_fullStr |
2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network |
title_full_unstemmed |
2D inverse modeling of the gravity field due to a chromite deposit using the Marquardt’s algorithm and forced neural network |
title_sort |
2d inverse modeling of the gravity field due to a chromite deposit using the marquardt’s algorithm and forced neural network |
publisher |
General Directorate of Mineral Research and Exploration |
series |
Bulletin of the Mineral Research and Exploration |
issn |
0026-4563 |
publishDate |
2020-04-01 |
description |
In this paper, two modeling method are employed. First, a method based on the Marquardt’s algorithm is presented to invert the gravity anomaly due to a finite vertical cylinder source. The inversion outputs are the depth to top and bottom, and radius parameters. Second, Forced Neural Networks (FNN) for interpreting the gravity field as try to fit the computed gravity in accordance with the estimated subsurface density distribution to the observed gravity. To evaluate the ability of the methods, those are employed for analyzing the gravity anomalies from assumed models with different initial parameters as the satisfactory results were achieved. We have also applied these approaches for inverse modeling the gravity anomaly due to a Chromite deposit mass, situated east of Sabzevar, Iran. The interpretation of the real gravity data using both methods yielded almost the same results. |
topic |
chromite deposit forced neural networks marquardt’s algorithm finite vertical cylinder gravity |
url |
http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/589224?publisher=mta |
work_keys_str_mv |
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1724858601819865088 |