The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland

The Koillismaa-Näränkävaara complex in North-eastern Finland is currently studied with a variety of geophysical and geochemical investigations to better understand its geological history and assess its mineral potential. The area is characterized by an East-West oriented deeply seated ultramafic int...

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Main Authors: Patzer, C., Autio, U., Kamm, J.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017702
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017702 2023-06-11T04:15:19+02:00 The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland Patzer, C. Autio, U. Kamm, J. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017702 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1875 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017702 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1875 2023-05-28T23:39:14Z The Koillismaa-Näränkävaara complex in North-eastern Finland is currently studied with a variety of geophysical and geochemical investigations to better understand its geological history and assess its mineral potential. The area is characterized by an East-West oriented deeply seated ultramafic intrusion within the granitoid bedrock which has been indicated by gravity and magnetic anomalies as well as 2D inversion of sparse magnetotelluric (MT) data. It was successfully drilled at a depth of 1.5 km by the Koillismaa Deep Hole. The aim of this study is to better delineate the geological structure around the Koillismaa Deep Hole area. We collected 70 MT sites along an approximately 40 km long profile across the intrusion. In addition, we also tested our newly acquired EM transmitter and collected a densely sampled controlled source AMT (CSAMT) profile across the Koillismaa Deep Hole at the centre of the MT profile. Data analysis of the MT data shows prominent geoelectrical strike direction perpendicular to the intrusion. However, it also shows a change of strike direction with depth by 20 ◦ . We will discuss possible causes of observed anisotropy and show inversion results of the MT data and compare it with latest results from our CSAMT survey. Our EM results will be further compared to other existing geophysical data such as borehole logs, gravity, and magnetic modelling as well as petrophysical measurements of the drill core. Conference Object Northern Finland GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Koillismaa ENVELOPE(29.047,29.047,65.843,65.843)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The Koillismaa-Näränkävaara complex in North-eastern Finland is currently studied with a variety of geophysical and geochemical investigations to better understand its geological history and assess its mineral potential. The area is characterized by an East-West oriented deeply seated ultramafic intrusion within the granitoid bedrock which has been indicated by gravity and magnetic anomalies as well as 2D inversion of sparse magnetotelluric (MT) data. It was successfully drilled at a depth of 1.5 km by the Koillismaa Deep Hole. The aim of this study is to better delineate the geological structure around the Koillismaa Deep Hole area. We collected 70 MT sites along an approximately 40 km long profile across the intrusion. In addition, we also tested our newly acquired EM transmitter and collected a densely sampled controlled source AMT (CSAMT) profile across the Koillismaa Deep Hole at the centre of the MT profile. Data analysis of the MT data shows prominent geoelectrical strike direction perpendicular to the intrusion. However, it also shows a change of strike direction with depth by 20 ◦ . We will discuss possible causes of observed anisotropy and show inversion results of the MT data and compare it with latest results from our CSAMT survey. Our EM results will be further compared to other existing geophysical data such as borehole logs, gravity, and magnetic modelling as well as petrophysical measurements of the drill core.
format Conference Object
author Patzer, C.
Autio, U.
Kamm, J.
spellingShingle Patzer, C.
Autio, U.
Kamm, J.
The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland
author_facet Patzer, C.
Autio, U.
Kamm, J.
author_sort Patzer, C.
title The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland
title_short The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland
title_full The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland
title_fullStr The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland
title_full_unstemmed The electrical conductivity structure beneath the Koillismaa-Näränkävaara complex in northern Finland
title_sort electrical conductivity structure beneath the koillismaa-näränkävaara complex in northern finland
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017702
long_lat ENVELOPE(29.047,29.047,65.843,65.843)
geographic Koillismaa
geographic_facet Koillismaa
genre Northern Finland
genre_facet Northern Finland
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1875
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017702
op_doi https://doi.org/10.57757/IUGG23-1875
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