Physical analysis of an Antarctic ice core—towards an integration of micro- and macrodynamics of polar ice

• Published in: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
• Main Authors: Weikusat, Ilka, Jansen, Daniela, Binder, Tobias, Eichler, Jan, Faria, Sérgio H., Wilhelms, Frank, Kipfstuhl, Sepp, Sheldon, Simon, Miller, Heinrich, Dahl-Jensen, Dorthe, Kleiner, Thomas
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: The Royal Society Publishing 2017
• Subjects: Antarc*; Antarctic; Antarctica; DML; Dronning Maud Land; ice core
• Online Access: https://epic.awi.de/id/eprint/42978/; https://epic.awi.de/id/eprint/42978/1/Weikusat2017.pdf; https://doi.org/10.1098/rsta.2015.0347; https://hdl.handle.net/10013/epic.49522; https://hdl.handle.net/10013/epic.49522.d001

Microstructures from deep ice cores reflect the dynamic conditions of the drill location as well as the thermodynamic history of the drill site and catchment area in great detail. Ice core parameters (crystal lattice-preferred orientation (LPO), grain size, grain shape), mesostructures (visual stratigraphy) as well as borehole deformation were measured in a deep ice core drilled at Kohnen Station, Dronning Maud Land (DML), Antarctica. These observations are used to characterize the local dynamic setting and its rheological as well as microstructural effects at the EDML ice core drilling site (European Project for Ice Coring in Antarctica in DML). The results suggest a division of the core into five distinct sections, interpreted as the effects of changing deformation boundary conditions from triaxial deformation with horizontal extension to bedrock-parallel shear. Region 1 (uppermost approx. 450 m depth) with still small macroscopic strain is dominated by compression of bubbles and strong strain and recrystallization localization. Region 2 (approx. 450{\textendash}1700 m depth) shows a girdle-type LPO with the girdle plane being perpendicular to grain elongations, which indicates triaxial deformation with dominating horizontal extension. In this region (approx. 1000 m depth), the first subtle traces of shear deformation are observed in the shape-preferred orientation (SPO) by inclination of the grain elongation. Region 3 (approx. 1700{\textendash}2030 m depth) represents a transitional regime between triaxial deformation and dominance of shear, which becomes apparent in the progression of the girdle to a single maximum LPO and increasing obliqueness of grain elongations. The fully developed single maximum LPO in region 4 (approx. 2030{\textendash}2385 m depth) is an indicator of shear dominance. Region 5 (below approx. 2385 m depth) is marked by signs of strong shear, such as strong SPO values of grain elongation and strong kink folding of visual layers. The details of structural observations are compared with ...