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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
Post-glacial reactivation of the Bollnäs fault, central Sweden – a multidisciplinary geophysical investigation
Alireza Malehmir et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC C1321: 'Referee Comments', Egidio Armadillo, 09 Nov 2015 Printer-friendly Version 
AC C1976: 'Response to the reviewer's comments', Alireza Malehmir, 13 Feb 2016 Printer-friendly Version Supplement 
 
RC C1366: 'Geophysics, Tectonophysics', Anonymous Referee #2, 18 Nov 2015 Printer-friendly Version 
AC C1977: 'Response to the reviewer's comments', Alireza Malehmir, 13 Feb 2016 Printer-friendly Version Supplement 
CC BY 4.0
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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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