Articles | Volume 12, issue 4
https://doi.org/10.5194/se-12-1005-2021
https://doi.org/10.5194/se-12-1005-2021
Research article
 | 
30 Apr 2021
Research article |  | 30 Apr 2021

Emplacement of “exotic” Zechstein slivers along the inverted Sontra Graben (northern Hessen, Germany): clues from balanced cross sections and geometrical forward modeling

Jakob Bolz and Jonas Kley

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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 Jakob Bolz on behalf of the Authors (05 Jan 2021)
ED: Publish subject to technical corrections (18 Jan 2021) by Piotr Krzywiec
ED: Referee Nomination & Report Request started (18 Jan 2021) by Piotr Krzywiec
RR by Stefan Back (03 Feb 2021)
RR by Alexander Malz (08 Feb 2021)
RR by Andrzej Konon (09 Feb 2021)
ED: Publish subject to technical corrections (09 Feb 2021) by Piotr Krzywiec
ED: Publish subject to technical corrections (11 Feb 2021) by Susanne Buiter (Executive editor)
AR by Jakob Bolz on behalf of the Authors (18 Feb 2021)  Author's response   Manuscript 
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Short summary
To assess the role smaller graben structures near the southern edge of the Central European Basin System play in the basin’s overall deformational history, we take advantage of a feature found on some of these structures, where slivers from older rock units appear along the graben's main fault, surrounded on both sides by younger strata. The implications for the geometry of the fault provide a substantially improved estimate for the magnitude of normal and thrust motion along the fault system.