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3D modelling of the Onega Basin, northwestern Russia, from gravity and magnetic data and borehole information

Frey, M. and Ebbing, J. and Lepland, A. (2018):
3D modelling of the Onega Basin, northwestern Russia, from gravity and magnetic data and borehole information.
In: Norwegian Journal of Geology, 4 (98), pp. 1-12. Geological Society of Norway, ISSN 0029-196x, e-ISSN 0029-196x,
DOI: 10.17850/njg98-4-03,
[Article]

Abstract

The Palaeoproterozoic Onega Basin in northwestern Russia is an important geological archive for global events during oxygenation of Earth at 2.5–2.0 Ga. In this study, we make use of recent drilling results from the Fennoscandian Arctic Russia – Drilling Early Earth Project and the Onega Parametric Hole in combination with available gravity and magnetic data to illuminate the structure of the basin and its internal build-up. These drilling campaigns have provided new information on petrophysical properties (density, magnetic susceptibility) and stratigraphic thickness of the main horizons in the basin. We use this information in combination with gravity and magnetic data to construct a 3D crustal model of the basin with emphasis on its near-surface structure. Our near-surface structure is in agreement with previous findings and most of the gravity and magnetic anomalies are associated with known geological bodies. Modelling also suggests a lateral lithological subdivision of the upper Archaean crust into three parts. The central crust has a higher magnetic susceptibility of 0.12 (SI) and lower density of 2.7 g/cm3, while the surrounding upper crust in the western and eastern edge regions has a lower magnetic susceptibility of 0.075–0.1 (SI), but a slightly higher density of 2.75–2.8 g/cm3. One possible explanation for the differences is the presence of highly magnetised magmatic rocks in the centre of the Onega region caused by magmatic activity resulting in lava flows and comagmatic shallow intrusions during the early Palaeoproterozoic.

Item Type: Article
Erschienen: 2018
Creators: Frey, M. and Ebbing, J. and Lepland, A.
Title: 3D modelling of the Onega Basin, northwestern Russia, from gravity and magnetic data and borehole information
Language: English
Abstract:

The Palaeoproterozoic Onega Basin in northwestern Russia is an important geological archive for global events during oxygenation of Earth at 2.5–2.0 Ga. In this study, we make use of recent drilling results from the Fennoscandian Arctic Russia – Drilling Early Earth Project and the Onega Parametric Hole in combination with available gravity and magnetic data to illuminate the structure of the basin and its internal build-up. These drilling campaigns have provided new information on petrophysical properties (density, magnetic susceptibility) and stratigraphic thickness of the main horizons in the basin. We use this information in combination with gravity and magnetic data to construct a 3D crustal model of the basin with emphasis on its near-surface structure. Our near-surface structure is in agreement with previous findings and most of the gravity and magnetic anomalies are associated with known geological bodies. Modelling also suggests a lateral lithological subdivision of the upper Archaean crust into three parts. The central crust has a higher magnetic susceptibility of 0.12 (SI) and lower density of 2.7 g/cm3, while the surrounding upper crust in the western and eastern edge regions has a lower magnetic susceptibility of 0.075–0.1 (SI), but a slightly higher density of 2.75–2.8 g/cm3. One possible explanation for the differences is the presence of highly magnetised magmatic rocks in the centre of the Onega region caused by magmatic activity resulting in lava flows and comagmatic shallow intrusions during the early Palaeoproterozoic.

Journal or Publication Title: Norwegian Journal of Geology
Journal volume: 4
Number: 98
Publisher: Geological Society of Norway
Uncontrolled Keywords: gravity field, magnetic field, 3D modelling, borehole data, Onega Basin
Divisions: 11 Department of Materials and Earth Sciences
11 Department of Materials and Earth Sciences > Earth Science
11 Department of Materials and Earth Sciences > Earth Science > Geothermal Science and Technology
Date Deposited: 22 Jan 2020 06:32
DOI: 10.17850/njg98-4-03
Official URL: https://njg.geologi.no/vol-91-100/details/1/2189-2189
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