view article

Figure 6
(a) X-ray diffraction pattern of a highly mineralized fish bone particle. The diffraction pattern, displayed on a logarithmic scale, extends to Q = 0.26 nm−1 at the edges. (b) The reconstructed image from (a) where the striations represent the mineralized fibrils.

Journal logoJOURNAL OF
SYNCHROTRON
RADIATION
ISSN: 1600-5775
Follow J. Synchrotron Rad.
Sign up for e-alerts
Follow J. Synchrotron Rad. on Twitter
Follow us on facebook
Sign up for RSS feeds