Decomposition of the gravitational field inversion using the assembly method for the ore model

The paper presents consideration of the solution of the nonlinear inverse problem of gravity exploration in the grid class of field sources if there are anomalies in the section that have positive and negative effective densities. In this case, practical equivalence is very strong and the reliabilit...

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Main Author: Dolgal, A.S.
Format: Article
Language:Russian
Published: Institute of Volcanology and Seismology FEB RAS 2019-03-01
Series:Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
Subjects:
Online Access:http://www.kscnet.ru/journal/kraesc/article/viewFile/233/pdf
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spelling doaj-a743a4c5918d4b51ae68684e69134cc52020-11-25T01:58:09ZrusInstitute of Volcanology and Seismology FEB RASВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле1816-55241816-55322019-03-01411253610.31431/1816-5524-2019-1-41-25-36Decomposition of the gravitational field inversion using the assembly method for the ore modelDolgal, A.S.0Mining Institute of the Ural Branch of the Russian Academy of Sciences, PermThe paper presents consideration of the solution of the nonlinear inverse problem of gravity exploration in the grid class of field sources if there are anomalies in the section that have positive and negative effective densities. In this case, practical equivalence is very strong and the reliability of the results of quantitative interpretation decreases. Based on the assembly method the author consideres the possibility of decomposing the inverse problem into two separate computational procedures. It is implemented using pre-separation of the gravitational field into components caused by objects with different effective densities. The author used a system of equivalent sources that were successively plunged to a depth approximating the interpreted field. Experiments showed that with a certain depth of sources, it is possible to rather accurately restore the «positive» and «negative» components. For each of them, the solution of the inverse problem is separately carried out, then the obtained results are synthesized, i.e. the construction of a unified geodensity model, which makes it possible to provide complete automation of additive interpretation technologies. The paper includes model examples illustrating the proposed approach.http://www.kscnet.ru/journal/kraesc/article/viewFile/233/pdfgravity surveyinterpretationinverse problemdecompositioneffective density
collection DOAJ
language Russian
format Article
sources DOAJ
author Dolgal, A.S.
spellingShingle Dolgal, A.S.
Decomposition of the gravitational field inversion using the assembly method for the ore model
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
gravity survey
interpretation
inverse problem
decomposition
effective density
author_facet Dolgal, A.S.
author_sort Dolgal, A.S.
title Decomposition of the gravitational field inversion using the assembly method for the ore model
title_short Decomposition of the gravitational field inversion using the assembly method for the ore model
title_full Decomposition of the gravitational field inversion using the assembly method for the ore model
title_fullStr Decomposition of the gravitational field inversion using the assembly method for the ore model
title_full_unstemmed Decomposition of the gravitational field inversion using the assembly method for the ore model
title_sort decomposition of the gravitational field inversion using the assembly method for the ore model
publisher Institute of Volcanology and Seismology FEB RAS
series Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
issn 1816-5524
1816-5532
publishDate 2019-03-01
description The paper presents consideration of the solution of the nonlinear inverse problem of gravity exploration in the grid class of field sources if there are anomalies in the section that have positive and negative effective densities. In this case, practical equivalence is very strong and the reliability of the results of quantitative interpretation decreases. Based on the assembly method the author consideres the possibility of decomposing the inverse problem into two separate computational procedures. It is implemented using pre-separation of the gravitational field into components caused by objects with different effective densities. The author used a system of equivalent sources that were successively plunged to a depth approximating the interpreted field. Experiments showed that with a certain depth of sources, it is possible to rather accurately restore the «positive» and «negative» components. For each of them, the solution of the inverse problem is separately carried out, then the obtained results are synthesized, i.e. the construction of a unified geodensity model, which makes it possible to provide complete automation of additive interpretation technologies. The paper includes model examples illustrating the proposed approach.
topic gravity survey
interpretation
inverse problem
decomposition
effective density
url http://www.kscnet.ru/journal/kraesc/article/viewFile/233/pdf
work_keys_str_mv AT dolgalas decompositionofthegravitationalfieldinversionusingtheassemblymethodfortheoremodel
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