Anisotropy and structure of the Priestley Glacier shear margin, Antarctica
We aim to use seismology to constrain the large scale crystallographic preferred orientation (CPO = crystal orientation fabric) across the Priestley Glacier shear margin and satellite data to model the strain history that has resulted in the CPO. We will compare these data to results of thermo-mecha...
Main Authors: | , |
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Format: | Dataset |
Language: | unknown |
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International Federation of Digital Seismograph Networks
2019
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Subjects: | |
Online Access: | https://dx.doi.org/10.7914/sn/zb_2019 https://www.fdsn.org/networks/detail/ZB_2019/ |