Articles | Volume 11, issue 4
Solid Earth, 11, 1489–1510, 2020

Special issue: Inversion tectonics – 30 years later

Solid Earth, 11, 1489–1510, 2020

Research article 11 Aug 2020

Research article | 11 Aug 2020

Pre-inversion normal fault geometry controls inversion style and magnitude, Farsund Basin, offshore southern Norway

Thomas B. Phillips et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Thomas Phillips on behalf of the Authors (12 Jun 2020)  Author's response
ED: Publish as is (02 Jul 2020) by Jonas Kley
ED: Publish subject to technical corrections (03 Jul 2020) by Susanne Buiter(Executive Editor)
Short summary
Normal faults often reactivate under compression, in a process called inversion. The 3D geometry of these structures (and the effect on resultant inversion structural style) is often not considered. Using seismic reflection data, we examine how stresses form different inversion styles that are controlled by the geometry of the pre-existing structure. Geometrically simple faults are preferentially reactivated; more complex areas are typically not reactivated and instead experience bulk uplift.