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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. (2015BB2)] 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.

Journal logoSTRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS
ISSN: 2052-5206
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