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Volume 7, issue 2 | Copyright
Solid Earth, 7, 509-527, 2016
https://doi.org/10.5194/se-7-509-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Apr 2016

Research article | 06 Apr 2016

Post-glacial reactivation of the Bollnäs fault, central Sweden – a multidisciplinary geophysical investigation

Alireza Malehmir et al.
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Cited articles
Ahmadi, O., Juhlin, C., Ask, M., and Lund, B.: Revealing the deeper structure of the end-glacial Pärvie fault system in northern Sweden by seismic reflection profiling, Solid Earth, 6, 621–632, https://doi.org/10.5194/se-6-621-2015, 2015.
Albrecht, L. and Kübler, L.: Bedrock Map 15G Bollnäs, scale 1 : 250 000, Geological Survey of Sweden, K312, 2011.
Arvidsson, R.: Fennoscandian earthquakes: whole crustal rupturing related to postglacial rebound, Science, 274, 744–746, 1996.
Bastani, M.: EnviroMT- A New Controlled Source/Radio Magnetotelluric System, PhD thesis, Acta Universitatis Upsaliensis, Uppsala Dissertations from the Faculty of Science and Technology 32, 2001.
Bastani, M., Malehmir, A., Ismail, N., Pedersen, L. B., and Hedjazi, F.: Delineating hydrothermal stockwork copper deposits using controlled-source and radio-magnetotelluric methods: A case study from northeast Iran, Geophysics, 74, B167–B181, 2009.
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Short summary
Glacially induced intraplate faults are conspicuous and confined to northern parts of Fennoscandia. Here we report a multidisciplinary geophysical investigation delineating the newly inferred lidar imagery data from the Bollnäs post-glacial fault in central Sweden. The geophysical data consistently support the presence of a fault in the crystalline basement associated with an earlier structure, possibly a deformation zone that reactive after the Weichselian deglaciation.
Glacially induced intraplate faults are conspicuous and confined to northern parts of...
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