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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Main Authors: Ata ESHAGHZADEH, Sanaz SEYEDI SAHEBARI, Alireza DEHGHANPOUR
Format: Article
Language:English
Published: General Directorate of Mineral Research and Exploration 2020-04-01
Series:Bulletin of the Mineral Research and Exploration
Subjects:
Online Access:http://dergipark.org.tr/tr/pub/bulletinofmre/issue/42676/589224?publisher=mta
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spelling 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 AT ataeshaghzadeh 2dinversemodelingofthegravityfieldduetoachromitedepositusingthemarquardtsalgorithmandforcedneuralnetwork
AT sanazseyedisahebari 2dinversemodelingofthegravityfieldduetoachromitedepositusingthemarquardtsalgorithmandforcedneuralnetwork
AT alirezadehghanpour 2dinversemodelingofthegravityfieldduetoachromitedepositusingthemarquardtsalgorithmandforcedneuralnetwork
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