15 Aug 2019
| 15 Aug 2019
Micromorphology and clast microfabrics of subglacial traction tills at the sea cliff Dwasieden: evidence of polyphase syn- and post-depositional deformation
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Cited articles
Beiche, T.: Microfacies and depositional environment of Weichselian
silt-clay rhythmites at the coastal cliff of Dwasieden (Jasmund, Rügen,
Pomerania), Master-Thesis, University of Greifswald, 1–58, Greifswald,
2014.
Brumme, J.: Three-dimensional microfabric analyses of Pleistocene tills from
the cliff section Dwasieden on Rügen (Baltic Sea Coast):
Micromorphological evidence for subglacial polyphase deformation, Doctoral
thesis, University of Greifswald, 1–250, 2015.
Evans, D. J. A., Phillips, E. R., Hiemstra, J. F., and Auton, C. A.: Subglacial
till: Formation, sedimentary characteristics and classification,
Earth-Sci. Rev., 78, 115–176, 2006.
Gehrmann, A.: The multi-stage structural development of the Upper
Weichselian Jasmund glaciotectonic complex (Rügen, NE Germany), Doctoral
thesis, University of Greifswald, 1–235, 2018.
Gehrmann, A. and Harding, C.: Geomorphological mapping and spatial analyses of
an Upper Weichselian glacitectonic complex based on LiDAR data, Jasmund
Peninsula (NE Rügen), Germany, Geosciences 8, 208,
https://doi.org/10.3390/geosciences8060208, 2018.
