Articles | Volume 2
15 Aug 2019
 | 15 Aug 2019

The sea cliff at Dwasieden: soft-sediment deformation structures triggered by glacial isostatic adjustment in front of the advancing Scandinavian Ice Sheet

Małgorzata Pisarska-Jamroży, Szymon Belzyt, Andreas Börner, Gösta Hoffmann, Heiko Hüneke, Michael Kenzler, Karsten Obst, Henrik Rother, Holger Steffen, Rebekka Steffen, and Tom van Loon

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Cited articles

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Brandes, C., Polom, U., and Winsemann, J.: Reactivation of basement faults: interplay of ice-sheet advance, glacial lake formation and sediment loading, Basin Res., 23, 53–64, 2011. 
Brandes, C., Winsemann, J., Roskosch, J., Meinsen, J., Tanner, D. C., Frechen, M., Steffen, H., and Wu, P.: Activity along the Osning Thrust in central Europe during the Lateglacial: Ice-sheet and lithosphere interactions, Quaternary Sci. Rev., 38, 49–62, 2012. 
Brandes, C., Steffen, H., Sandersen, P. B. E., Wu, P., and Winsemann, J.: Glacially induced faulting along the NW segment of the Sorgenfrei-Tornquist Zone, northern Denmark: implications for neotectonics and Lateglacial fault-bound basin formation, Quaternary Sci. Rev., 189, 149–168, 2018. 
Brumme, J., Hüneke, H., and Phillips, E.: Micromorphology and clast microfabrics of subglacial traction tills at the sea-cliff Dwasieden: evidence of polyphase syn- and post-depositional deformation, DEUQUA Spec. Pub., this volume, 2019.