Sea cliff at Wissower Bach (Pleistocene stripe 5) – microstructural evidence of large-scale glacitectonism and glacier kinematics

Gehrmann, Anna; Hüneke, Heiko; Meschede, Martin; Phillips, Emrys. 2019 Sea cliff at Wissower Bach (Pleistocene stripe 5) – microstructural evidence of large-scale glacitectonism and glacier kinematics. DEUQUA Special Publications, 2. 29-33. https://doi.org/10.5194/deuquasp-2-29-2019

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Official URL: http://dx.doi.org/10.5194/deuquasp-2-29-2019

Abstract/Summary

Soft-sediment thin sections from a SW-dipping thrust fault at the south-western limb of the Wissower Bach syncline (NE Rügen) give rise to the complicated glacitectonic environment in the south-western Baltic Sea region. Micromorphology, microstructural mapping, and macroscale information have led to the development of a detailed model for the evolution of the syncline during late Weichselian glacitectonism

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.5194/deuquasp-2-29-2019
ISSN:	2625-8137
Date made live:	19 Aug 2019 11:40 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/524805

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.5194/deuquasp-2-29-2019

ISSN:

2625-8137

Date made live:

19 Aug 2019 11:40 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/524805