Full-field predictions of ice dynamic recrystallisation under simple shear conditions
详细信息    查看全文
文摘

Lattice preferred orientation is not strongly affected by recrystallisation.

Ice crystal intrinsic anisotropy is transferred to the polycrystalline scale.

LPOs and SPOs control strain hardening and subsequent softening.

Strain localisation bands are masked by grain boundary migration.

Masked strain localisation can be recognised from polar ice microstructures.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700