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16 - Glacially Induced Faults in Germany

from Part IV - Glacially Triggered Faulting at the Edge and in the Periphery of the Fennoscandian Shield

Published online by Cambridge University Press:  02 December 2021

By
Katharina Müller ,
Jutta Winsemann ,
David C. Tanner ,
Thomas Lege ,
Thomas Spies  and
Christian Brandes
Edited by
Holger Steffen ,
Odleiv Olesen  and
Raimo Sutinen
Holger Steffen
Affiliation:
Lantmäteriet, Sweden
Odleiv Olesen
Affiliation:
Geological Survey of Norway
Raimo Sutinen
Affiliation:
Geological Survey of Finland
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Summary

Recent studies have shown that the low seismicity of northern Germany is characterized by fault activity caused by the decay of the Late Pleistocene (Weichselian) ice sheet. Several faults and fault systems show evidence of neotectonic activity, all of which are oriented parallel to the margin of the Pleistocene ice sheets. The timing of fault movements implies that the seismicity in northern Germany is likely induced by varying lithospheric stress conditions related to glacial isostatic adjustment, and the faults thus can be classified as glacially induced faults. For the Osning, Harz Boundary and Schaabe faults, this is supported by numerical simulation of glacial isostatic adjustment-related stress field changes. Glacial isostatic adjustment is also a likely driver for the historical and parts of the recent fault activity. Glacial isostatic adjustment is also described for the Alps, but it is difficult to clearly distinguish between reactivation of faults in the foreland of the Alps due to the Alpine collision and glacial isostatic adjustment.

Keywords

Soft-Sediment Deformation StructuresGlacial Isostatic AdjustmentForebulgeNeotectonicsSeismicityCentral European Basin SystemOsning ThrustHarz Boundary FaultSchaabe FaultGermany
Type
Chapter
Information
Glacially-Triggered Faulting , pp. 283 - 303
Publisher: Cambridge University Press
Print publication year: 2021

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