Abstract
Transmission and back reflection X‐ray topographs of a large near (100) Fe‐3 wt% Si subgrain compressed along an easy surface direction of magnetization are taken with white synchrotron radiation. Disappearance of the [001] stripe domain contrast is observed only in the 001 transmission topograph. High resolution back reflection topographs reveal a zig‐zag fine structure of the stripes. A domain model to explain the results is presented.
Original language | English |
---|---|
Pages (from-to) | 495-500 |
Journal | Physica Status Solidi A: Applied Research |
Volume | 58 |
Issue number | 2 |
DOIs | |
Publication status | Published - 1980 |
MoE publication type | A1 Journal article-refereed |