In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 122, No. 9 ( 2017-09), p. 7076-7089
Abstract:
In situ measurements of elastic wave velocity evolution during the ductile deformation of ice can be used as a proxy for CPO evolution Weakening at almost equal to 3% axial shortening may result from connected networks of grains well oriented for basal slip in the macroscopic stress field CPO development starts at the onset of weakening; the evolution of CPO leads to significant mechanical weakening in vertical shortening
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1002/2017JB013964
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13