Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics

The efforts of today’s society to switch to greener technology and fossil-free energy requires mineral resources. The economical depth of new deposits grows hence deep exploration methods are needed. Magnetotellurics is non-invasive passive electromagnetic method allowing to survey from the surface...

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Main Authors: Rydman, O., Smirnov, M.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021708
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021708 2023-07-30T04:04:40+02:00 Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics Rydman, O. Smirnov, M. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021708 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4272 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021708 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4272 2023-07-16T23:40:25Z The efforts of today’s society to switch to greener technology and fossil-free energy requires mineral resources. The economical depth of new deposits grows hence deep exploration methods are needed. Magnetotellurics is non-invasive passive electromagnetic method allowing to survey from the surface down to a several tens of km and therefore is a choice when deposit scale information is required. In 2018 a magnetotelluric 3-D array dataset was collected around known magnetite-pegmatite-deposits in Kiruna, Sweden. The survey area is affected by industrial electromagnetic noise from the mine and Kiruna town, which is often a challenge for the magnetotelluric method. Nevertheless, we utilized robust multi-remote reference processing techniques to derive magnetotellurics transfer functions which are in general of a good quality, except a few sites. Many sites exhibit an unusual behavior with phase of main components of the impedance tensor going out of quadrant. This behavior can be indication of noisy data or possibly strong 3D effects. Therefore, we rely on data re-weighting scheme to conclude about the data quality. The final 3-D model was obtained after a few re-weighted least square iterations using diffusion smoothness constrains as model covariance matrix (Second order Tikhonov regularization). Finally, we have obtained a model with stable anomalies at all depths which matches known geology but brings new details and insights into the general understanding of the area. Conference Object Kiruna GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Kiruna
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The efforts of today’s society to switch to greener technology and fossil-free energy requires mineral resources. The economical depth of new deposits grows hence deep exploration methods are needed. Magnetotellurics is non-invasive passive electromagnetic method allowing to survey from the surface down to a several tens of km and therefore is a choice when deposit scale information is required. In 2018 a magnetotelluric 3-D array dataset was collected around known magnetite-pegmatite-deposits in Kiruna, Sweden. The survey area is affected by industrial electromagnetic noise from the mine and Kiruna town, which is often a challenge for the magnetotelluric method. Nevertheless, we utilized robust multi-remote reference processing techniques to derive magnetotellurics transfer functions which are in general of a good quality, except a few sites. Many sites exhibit an unusual behavior with phase of main components of the impedance tensor going out of quadrant. This behavior can be indication of noisy data or possibly strong 3D effects. Therefore, we rely on data re-weighting scheme to conclude about the data quality. The final 3-D model was obtained after a few re-weighted least square iterations using diffusion smoothness constrains as model covariance matrix (Second order Tikhonov regularization). Finally, we have obtained a model with stable anomalies at all depths which matches known geology but brings new details and insights into the general understanding of the area.
format Conference Object
author Rydman, O.
Smirnov, M.
spellingShingle Rydman, O.
Smirnov, M.
Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics
author_facet Rydman, O.
Smirnov, M.
author_sort Rydman, O.
title Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics
title_short Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics
title_full Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics
title_fullStr Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics
title_full_unstemmed Exploring Iron Ore deposit around Kiruna with 3-D magnetotellurics
title_sort exploring iron ore deposit around kiruna with 3-d magnetotellurics
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021708
geographic Kiruna
geographic_facet Kiruna
genre Kiruna
genre_facet Kiruna
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4272
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021708
op_doi https://doi.org/10.57757/IUGG23-4272
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