Lookup NU author(s): Dr Neil Ross
This work is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0).
It has been hypothesized that complex englacial structures identified within the East Antarctic and Greenland ice sheets are generated by (i) water freezing to the ice sheet base and evolving under ice flow, (ii) deformation of ice of varying rheology, or (iii) entrainment of basal material. Using ice-penetrating radar, we identify a widespread complex of deep-ice facies in West Antarctica that exist in the absence of basal water. These deep-ice units are extensive, thick (>500 m), and incorporate multiple highly reflective englacial layers. At the lateral margin of an enhanced flow tributary of the Institute Ice Stream, these units are heavily deformed and folded by the action of lateral flow convergence. Radar reflectivity analysis demonstrates that the uppermost reflector of the deep-ice package is highly anisotropic, due to abrupt alternations in crystal orientation fabric, and consequently will have a different rheology to the ice above and below it. Deformation and folding of the deep-ice package is an englacial response to the combination of laterally-convergent ice flow and the physical properties of the ice column.
Author(s): Ross N, Corr H, Siegert M
Publication type: Article
Publication status: Published
Journal: The Cryosphere
Print publication date: 30/06/2020
Online publication date: 30/06/2020
Acceptance date: 18/05/2020
Date deposited: 30/06/2020
ISSN (print): 1994-0416
ISSN (electronic): 1994-0424
Publisher: European Geosciences Union (EGU)
Data Source Location: https://data.bas.ac.uk/metadata.php?id=GB/
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