Figure 1
Diffuse scattering intensity maps for inorganically formed natural calcite in comparison to ab initio calculations [left column; for experimental and computational details see Bosak et al. (2015)] and for sea urchin spine (right column). Laue symmetry elements are applied to the reconstructed maps in order to remove the detector gaps. Combined linear greyscale/logarithmic colour scale visualization is applied to the experimental data. |