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...

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Bibliographic Details
Main Authors: David Prior, Huw Horgan
Format: Dataset
Language:unknown
Published: International Federation of Digital Seismograph Networks 2019
Subjects:
Online Access:https://dx.doi.org/10.7914/sn/zb_2019
https://www.fdsn.org/networks/detail/ZB_2019/