Converging flow and anisotropy cause large-scale folding in Greenland's ice sheet
A range of mechanisms has been proposed for large-scale folding in polar ice sheets. Here, using new three-dimensional reconstructions of such folds in the onset region of the Greenland Petermann Glacier, the authors show that these formed due to flow convergence and the high mechanical anisotropy o...
| Main Authors: | , , , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2016-04-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms11427 |